41J10MM01t2.157MMJBWEL 010

O

1570 8

REPORT OM Tint

GEOLOGY AMD COPPER-PRECIOUS METAL MIMERALIZATIOM

OM THE

JBMTIMA MIME PROPERTY

ALBAMEL ft MICHOLAS TOVMSHIPS

OMTARIO

FOR

A. J. ROY

TOBOITO, GHTASIO

15, 1994

V. O. VILLOUGHBY, B. Se. (BOBS. )

KK&J RBSODRCB ASSOCIATES LIMITED

Oil

2JUUABT

A program of geological napping and prospecting on the Jentlna Hine Property concentrated on the evaluation of two, east-west trending copper-precious metal structural zones.

The lo. l Copper-Precious Metal Structure Is delineated over a strike length of 3,500 feet and Is hosted mainly by Espanola Formation limestone. Yidth varies from 60 feet on the west to 150 feet on the east. The showing consists of a chalcopyrlte-bearing quartz-chlorlte -i-/- albite breccia hasted by a chloritic shear. Extensive albite-sllica alteration Is associated and later subparallel and cross-cutting quartz-carbonate veins are also mineralized.

Massive sulphide horizons In the Bo. l Structure occur In Pit l at the Main Showing In the east. An 8-foot channel sample containing some massive sulphide assayed 6.782 copper and 1.90 oz silver per ton. Gold values of up to 0.03 oz per ton were returned from some samples.

At the east end, channels from Trench l returned up to O.63* copper over 4 feet and O.4452 copper over 10 feet. Grab samples of mineralized rock returned up to 1.252 copper and 0.029 cz gold per ton. A 5-foot channel from Trench 2, 300 feet eas~ of Trench l, ran l.882 copper.

The Id. 2 Copper Structure consists of mainly quartz- carbonate veining hosted by sheared and chloritized Espanola Formation siltstone and Gowganda Formation conglomerate. To date, the zone measures 4,400 feet long (east-west). Due to poor exposure, the width Is not well defined. The host structure is on a line with the White River Lead Mine (Cu-Pb-Ag-Au-Zn-Co-Ei) , 3,000 feet to the west. To the east, the zone was not prospected beyond a 250-foot long area of trenching, and Is considered open in that direction.

The Southeast Trench gave 1.832 copper over a 4-foot channel of chalcopyrite-rich quartz veining. A grab of semi-massive chalcopyrite from a pit 250 feet to the west assayed 13.002 copper.

The mineralized structures are considered to represent a class of polymetallic quartz veins and/or Cu-Au-bearlng veins and breccia pipes commonly found within the Proterozoic Huronian Basin. They may be parallel or subsidiary faults to the Flack Lake Fault Zone, a reverse thrust fault which may be the northern boundary fault for the Huronian Basin. Archean basement racks outcrop to the north.

Other known copper-precious metal zones on the Jentlna Property Include the Canamiska Zone, a 9,600-foot long EM conductor and soil geochemical zone. The best reported drill intersection was 1.442 copper over 19.5 feet. Some narrower sections graded in excess of 42 copper.

Structural-mlneralcgic and aeromagnetic features at the No. l Copper-Precious Metal Structure suggest the most likely target for economic mineralization on the Jentlna ground Is polymetallic CCu-Ag Au) mineralized breccia zones or pipes similar to the Proterozoic Olympic Dam deposit in Australia and the Vernecke Mountains deposits of the Yukon.

Other possible mineral targets are high-grade polymetallic veins, a style which historically has produced, over 36,000 tons of copper plus some precious metals In the Huronian Basin, VMS- style deposits In either Huronian and/or Archean volcanics, Archean style lode gold mineralization along or subsidiary to the Flack Lake Fault System, and perhaps SEDEX mineralization.

A two phase exploration program, emphasizing structural mapping, lithogeochemical sampling and diamond drilling is proposed to test the various possible styles of mineralization on the Jentina Property. Estimated cost of this work is 4881,000.

4M10MWI0192.1SIWMBANB. 01OC

TABLE OP CONTENTS

SUMMARY

1.0 INTRODUCTION l

2.O PROPERTY AMD DESCRIPTION 22.1 Location, Access and Infrastructure 22.2 Claim Status 4

3.0 PREVIOUS VUKK. 73.1 Mining and Exploration Company Activity 7

3.1.1 Sudbury Basin Mines Limited, 1927-1929 73.1.2 A. H. Clark, 1956 93.1.3 Plcton Uranium Mines Ltd., 1955-1968 93.1.4 Brace-Presto Mines Ltd., 1964-1965 103.1.5 Canamiska Copper Mines Ltd., 1965 123.1.6 Hanna Mining Company, 1969 133.1.7 Paquette Claims, 1952-1965 143.1.8 Atlantic Richfield Co.,

Triller Explorations Ltd.. 1967-1968 143.1.9 Stanford Mines Limited, 1971-1972 15

3.1.10 Gowganda Silver Mines Limited, 1972 163.1.11 Fort Norman Explorations Inc., 1974-1975 173.1.12 Charles M. Mortimer, 1984 2O3.1.13 International Mine Services Ltd.. 1986 203.1.14 United Reef Petroleums Limited, 1988 20

3.2. Academic and Government Studies 22

3.2.1 Paul Scheerer, University of Wisconsin,1956 22

3.2.2 J.W. Gasch and T.A. Vogel, Universityof Wisconsin, 1959 23

3.2.3 Provincial Government Surveys 233.2.4 Federal Government Surveys 23

4.0 REGIONAL GEOLOGY AID MINERAL IZATIOI 254. l Geological and Structural Framework 254.2 Base Metal and Precious Production 324.3 Mineral Deposits 35

5.0 EXPLORATION MODEL 43 5. l Polymetallic Veins, Breccias and Breccia

Pipes 435.2 Volcanogenic Massive Sulphide Deposits 545.3 Archean Lode Gold Deposits 545.4 Exploration Techniques 55

6.0 GEOLOGICAL MAPPING AID SAMPLING PROGRAM 59

7. O EXPLORATION RESULTS 627.1 Preamble 627.2 Geology and Distribution of Lltaologlcal

Units 627.3 Structural Geology and Xlnerallzatlon 667.4 Copper and Precious Betals-Bearing Structures 69

7.4.1 Vo. l Copper-Precious Setal Structure 707.4.2 To. 2 Copper Structure 787.4.3 Concluding Remarks 83

8.0 COBCLUSIOBS 85

9. O RBCQOEFDATIOIS 88

CERTIFICATE OF QUALIFICATIONS

PLATES

APPETOICES

CERTIFICATES OP ABALYSIS

APS

LIST OP FIGURESpage

Figure 1: General Location lap 3

Figure 2: Claim lap 6

Figure 3: 8 General geology and adit workings at the Little White River Lead line (after loore, 1929)

Figure 4: 18Plan of trenching and drill hole locations at the lain Showing,Fort lorman Explorations (after Rupert, 1974)

Figure 5: 24 Regional total field magnetics covering the Jentlna Property

Figure 6: 26 Regional geology and mineral deposits (after Roscoe ft Card, 1992)

Figure 7: 27 Geological sketch map of the Huronian Basin showing elements of the Penokean Fold Belt (after Bennett et al. 1991)

Figure 8: 28 Schematic diagram illustrating the paleotectonic model proposed for the formation and deformation of the Huronian Basin (after Bennett et al, 1991)

Figure 9: 3O Chronology of deformation and metallogenic events in the Proterozoic Huronian Supergroup (after Fyon et al, 1992)

Figure 1O: 40 Copper deposits across Southern Province (after Pearson, 1979)

Figure 11: 41Gold and polymetallic mineral deposits in the Huronian BasinCafter Fyon et al. 1992)

Figure 12: 42 Locations of possible VIS and HKIIKI deposits in the Huronian Basin (after Fyon et al, 1992)

Figure 13: 45 Examples of vein filled fault or fracture breccias (after Laznlcka, 1988)

Figure 14: 46Fault breccia development governed by rock competency (afterLaznlcka, 1988)

Figure 15: 47 Breccia formation due to faulting and fracturing (after Laznlcka, 1988)

Figure 16: 48Morphology of a diatreme showing relative sites of possible

Qization (after Laznlcka, 1988)

Figure 17: 49 Morphology of mineralized breccia In host sediments at the Victoria Mine, levada (after Atkinson et al, 1982)

Figure 18: 50 Mineralized skarn breccia at the Victoria Mine, levada (after Atkinson et al, 1982)

Figure 19: 51 Schematic diagram of the form and structure of the Olympic Dam and Acropolis deposits, Australia after Hltzman et al, 1991)

Figure 20: 52 Schematic diagram showing form and alteration features of the sedimentary hosted vernecke Mountain type Cu Fe deposits (after Hitzaan et al, 1992)

Figure 21: 53 Tectonic setting of Olympic Dam-vernecke Mountain breccia style precious and base metal deposits (after Hltzman et al, 1992)

Figure 22: 57 Proterozoic volcanic hosted VMS deposits in the Snow Lake area, northern Manitoba (after Walford and Franklin, 1982)

Figure 23: 58 Section of the Anderson VMS Mine, Manitoba (after valford and Franklin, 1982)

Figure 24: 72 Trench l, east face: geology, sample sites and assay results

Figure 25: 75 Trench 2, east face: geology, sample sites and assay results

Figure 26: 76 Plan map of pits and trenches, Main Showing area

Figure 27: 77 Main Showing, Pit l, south face: geology, sample sites and results

A Figure 28: 81 . SB trench, neat face: geology, sample sites and assay results

LIST OF TABLES

Table 1: Table of Formations 31

Table 2: 33List of Copper ft Precious Metals Production in the SouthernProvince (excluding the Sudbury Basin and Keweenawan deposits)

Table 3: 34 Documented Copper Inventory in the Huronian Basin

Table 4: 39 Classification of Copper Deposits for the Huronian Basin (after Pearson. 1978, 1979)

Table 5: Table of Formations, Jentlna Hine Property 64

Table 6: 70 (Mineralized) breccia/vein zones and associated alteration

LIST OF APPEIDICES

APPEMDIZ A: Summary Diamond Drill LogsA. l Plcton Uranium Mines Ltd., 1955-1968 Al A.2 Canamlska Copper Mines Ltd., 1965 A2 A. 3 Hanna Mining Company, 1969 A10 A.4 Atlantic Rlchfiled Company, 1968 A1O A.5 Stanford Mines Limited, 1971-1972 All

APPEMDIZ B: Diamond Drill Logs, Fort Morman Rxplorations Inc., 1974

APPEMDIZ C: 1988 Rock Sample Descriptions and Analytical Results, United Reef Petroleums Limited

APPEMDIZ D: 1993 Rock Sample Descriptions and Analytical Results

APPEMDIZ B: 1994 Rock Sample Descriptions and Analytical Results

LIST OF HAPS

Hap la: Area Geology, Structures and Mineral Occurrences; Albanel Twp. (scale, 1:2O,OOO)

Hap Ib: Area Geology, Structures and Mineral Occurrences; nicholas Twp. (scale, 1:2O,OOO)

Map A: Exploration Data Compilation, ^"" " g*-** Copper Mines Ltd. , 1965 (scale, l* ~ 500* )

Geology and KLneral Structure laps W9 Sheet S9 Sheet B Sheet SB Shoot

(scale l" = 20O')

LIST OF PLATES

Plate 1:View south of Nipissing diabase ridge at approximately L64+OOW,17+OOS C*94 grid)

Plate 2:Exposed ridge of Gowganda Formation arkosic sandstone with somegranite pebbles; at L24+OOW. 3+OOS C*94 grid)

Plate 3:View to northwest of Bndakal Lake; from the position of Plate 2

Plate 4:View north-northwest of Archean granite along the trace of the Flack Lake Fault, north of the Little White River; from the position of Plate 2

Plate 5:Ripple marks and some slump folding In Bar River Formationquartzite at L25+OOE. 7+5OS C*93 grid)

Plate 6:View west of the Bailey bridge across the Little White River;from the position of Plate 5

Plate 7:Ridge of Klsslssagl Formation sandstone north of the Little WhiteRiver; view north from the position of Plate 5 .

Plate 8:Graded bedding in Gowganda Formation arkosic sandstone/quartzite at approximately L12+OOW. 2+75S C'94 grid); stratIgrahlc tops are indicated to be overturned to the north

Plate 9:Slump features In Gowganda Formation heterolithic conglomerate along the property access road at approximately L36+OOW, TL12+OO1" C*94 grid)

Plate 10:The author standing at the east face. Trench l, of Mineralized quartz chlorite albite breccia and quartz carbonate vein zone in host Espanola Formation limestone and siltstone. Channel samples sites 9402 to the left CO.2851 Cu over 6.0 ft.) and 9403 to the right (0.335* Ga over 5.0 ft.)

Plate 11:Chris Xarchildon measuring strike and dip of siltstone strata (bottom) at the east face, Trench 1. The siltstone is overlain by sulphide rich quartz chlorite +S— albite breccia and altered limestone/siltetone. Channel sample site 9405 (0.093Z Cu over 6.0 ft.) is displayed

Plate 12:Typical quartz chlorite breccia in Trench la at approximately L1+5OV, TL10+OOM O93 grid); Malachite-staining with chalcopyrite blebs show preference for cross cutting fracture pli

Plate 13:Chris standing at the east end, south face of Pit l, the Main Showing; channel sample sites 9423 (1.35* Cu over 9.0 ft.) to the left and 9422 (6.78* Cu, 1.90 oz Ag/T and 195 ppb Au over 8.O ft.) to the right

Plate 14:At the went end, sooth face Pit l with channel sample sites 9424 (O.80* Cu and l,OSO ppb Au over 6.0 ft.) to the left, sample site 9425 (l.OO* Cn over 9.0 ft.) to the right

Plate 15:Close up of sample site 9422 showing massive sulphide (pyrite chalcopyrite bornite) horizon at lower right and folded Espanola Formation limcotone/slltstone at upper right

Plate 16:Chloritic shear zone at sample site 9423 showing malachite- staining and chalcopyrite bearing *aii***T- parallel and oblique quartz velnlets

Plate 17:View of the west face of the Southeast Trench, 1st terrace, atapproximately L3+5OV, 4-H5OS C94 grid). Chip channel sample site9441 (1.83* Cu over 4.0 ft.) across the main sulphide-bearing quartz vein; chloritic shear zone on either side and with some quartz chlorite breccia

Plate 18:View of the west face of the Southeast trench, 2nd terrace, 15ft. east of the location of Plate 17. Chip channel sample site9442 returned 1.22* Cn over 6.0 ft.r

-i-

1.0 I1TKODUCTIOM

Sporadic exploration has been carried out in the property

area for a number of years targeting what were referred to as

mineralized quartz veins. Exploration activity and provincial

government surveys In the Huronian in the Sudbury area in recent

years, plus research and property visits by the author in and

around the property area, indicate that particular structural and

alteration features characterize the Huronian Basin deposits,

such as regional fault zones, occurrences of mineralized breccia

pipes and associated albitization, and that such features have

largely been un-recognized or Ignored in the region west of

Sudbury.

The emerging consensus is that regional fault patterns and

Increasingly recognized zones of deformation have played a major

role in metallic mineral deposition and that recognition of

structure and alteration may lead to the discovery of significant

economic deposits. The fact that most researchers consider the

Huronian-Archean Interaction to be one of continental collision-

subduct ion zone mechanics conjures epithermal (Cordilleran-type)

and mesothermal (Archean-style) models as applicable to the

Huronian Basin.

This report on the current and historical exploration work

on the Jentina project and environs describes the field mapping y

prospecting results and reflects on the regional structural

context of Jentina copper-precious metal mineralization.

-2-

2.0 PROPERTY DESCRIPTION AID LOCATION

2. l Location, Access and Infrastructure

The Jentlna mineral property Is located In central east

Albanel Township and central west Nicholas Township, District of

Algoma, Sault Ste. Marie Mining Division, Ontario (Figure 1). The

main claim block fallows, and in places contains, some 4 Km of

length of the westerly flowing Little White River. All weather

secondary Highway 546 follows the course of the river, crossing

the northern part of the main claim block. This route connects

the property to Iron Bridge to the southwest, some 45 Km and to

Elliot Lake, 50 Km southeast.

The property is covered by well forested, steep-sided east-

west running outcrop ridges with elevations of up to 1,500 feet.

Numerous denuded rock promlnatories provide many scenic vistas.

The main forest cover consists of poplar with some scattered

stands of pine and maple. Timber on portions of the western part

of the property was harvested in 1989.

Numerous CATV) trails and roads, some in consequence of the

logging operation, provide access to the western part of the

property, particularlly from the Vhlte River Lodge. The lodge is

located 200 m west of the claim block and was used as a base for

the field mapping/prospecting program.

Access to the eastern part of the claim block was provided

by an AT7 trail from the Vhlte River Lodge which swings south of

Le Scarbo Lake and east to the eastern property boundary. A trail

extends south from this route to the Vhite River, close to the

-3-

Flgure 1: General location map

-4-

Albanel Vlcholas township boundary. A logging road running

north from Highway 546 extends just west of the northern claim

group.

The uranium mining town of Billot Lake, with a population of

13,500, Is the closest available centre for mining and

development services and supplies as well as possible custom

milling facilities. At present, there Is no electrical power

source In the region of the Jentina Property.

2.2 Claim Stati

The property comprises seventeen (17) unpatented mining

claims In two (2) blocks, one of fifteen (15) and another of two

(2) contiguous claim groups (Figure 2); all claims are held in

the name of Arthur J. Soy. The total area of the property Is

approximately 1,600 hectares. Recording dates for the filing of

mining assessment work on the claims Is as follows:

Main Group (15 claims - Albanel ft nicholas)

Claim To. Recording Date Assessment Due By

1197219 17 Dec, 1992 17 Dec, 19941197220 17 Dec, 1992 17 Dec, 19941197221 17 Dec, 1992 17 Dec, 19941118613 3 Hay, 1993 3 May, 19951118612 3 May, 1993 3 May, 19951118693 20 Jan, 1994 20 Jan, 19961118694 20 Jan, 1994 20 Jan, 19961118695 20 Jan, 1994 20 Jan, 19961118696 20 Jan, 1994 20 Jan, 19961118697 20 Jan, 1994 20 Jan, 19961186886 5 Apr, 1994 5 Apr, 19961186887 5 Apr, 1994 5 Apr, 19961186888 5 Apr, 1994 5 Apr, 19961186889 5 Apr. 1994 5 Apr, 19961197740 9 Jun, 1994 9 Jun, 1996

-5-

Trlangle Lake Group (Albanel A Hi. cho las)

Clala Id. Recording Date * —— —tar lil Due By

1118633 25 lov, 1993 25 lov, 19951118634 25 Ibv, 1993 25 Jov, 1995

-6-

Figure 2: Claim nap

r -7-3.0 PREVIOUS 1GKK

3.l lining and. Exploration Company Activity

3.1.1 Sudbury Basin Mines Limited. 1927-1929

Sudbury Basin Mines held a block of 16 claims in the Le

Scarbo Lake area, the White Blver Lead Mine. Currently five

patent claims cover the Mine area and are owned by Falconbridge

Limited. The patents are enclosed to the north, east and west by

the Jentlna Property.

Considerable pitting and trenching was carried out exposing

a 500-foot long, north-south trending sulphide-bearing quartz

vein zone hosted by Nipissing diabase (Figure 3). The main vein,

which measures up to 14 feet wide < Moor e, 1929), dips 45 deg

easterly. The vein was further prospected by a 175—foot long adit

with 354 feet of crosscutting (Shklanka, 1969). The adit was

driven Into the east side the steep diabase hill, 35 feet from Le

Scarbo Lake (Moore, 1929). The adit is now covered and the exact

location is not known (Willoughby, this report). Chalcopyrite,

pyrite, galena and pyrrhotite are the main sulphides. Some east-

west veins are also reported (Moore, 1929).

A grab sample of the main vein from a pit assayed 2.6 oz

Ag/T, 3.1* Cu, 20.6* Pb (Moore, 1929). Shklanka (1969) reported

that one of 5 grab samples of quartz vein material in the dump

returned 0.10 oz Au/T, 3.46 oz Ag/T, 1.56* Cu, 0.63* Pb, 0.26*

Zn, 0.1* Co and 0.05* Bi.

V---'-- 2-- V V

v v

V

V

i w - - f .j -' * * v vp *J * v w * l |v

"5601

Scale. 20 Chajns-1 Inch

Figure 3: General geology and. ad.lt Blver Lead Mine (after

kinge at the Little White 1929)

3.1.2 A. H. Clark, 1956

Mr. Clark, a prospector, uncovered some copper

mineralization in a shear zone on a steep rock face north of and

overlooking the Little White River at a position approximately

1,000 feet west of the Highway 546 bailey bridge. This falls

within or close to the northwestern corner of Jentlna Block

1118612 (Figure 2, Map la). Siemiatkowska reports the

mineralization is contained in a horizontal, chloritlzed shear

zone trending 040 deg close to or within the trace of the

regional Flack Lake Fault and hosted by nipissing diabase (1978).

ffumerous quartz-carbonate -l-/- feldspar, epidote veins measure up

to l—foot wide and contain narrow fractures containing

chalcopyrite with some pyrite and specularite. Clark's sampling

returned 0.62ft Cu in a grab.

3.1.3 Picton Uranium lines Ltd., 1955-1968

The company carried out uranium exploration including

geological mapping and diamond drilling over central-east Albanel

Township covering the northern part of the Jentlna Main Claim

Block, north to Speckle Lake. A total of 1,629 ft. of drilling in

four holes were completed north of the Little White Biver. Three

of the holes (l to 3) apparently targeted Klsslssagi Formation

quartz pebble sandstone and conglomerate. Uranium assays were

low. Some diabase was intersected. Hole 4, a vertical hole

situated north of Speckle Lake, reported quartzite (Bar Blver

Formation?) and interbedded siltstone/arglllite. Some hematite

-10-

was noted in all of the holes, however no mention of sulphide

mineralization was made. Hole locations are shown on Map la.

Albanel. Summary logs are presented in Appendix A.

3.1.4 Brace-Presto Mines Ltd., 1964-1965

The company carried out geological mapping, IP surveying and

diamond drilling on a block of claims In Nicholas Township

located 300 feet south of a copper-cobalt showing on patent claim

87P. The Bruce-Presto group Is covered by the eastern part of the

Jentlna Main claim block. Apparently, the patent claims to the

north were also surveyed geophysically by Bruce-Presto.

The exploration work was directed by D.C. McEechnle, P.Eng.,

who also directed a program of trenching and drilling on the

patent claim in 1952. He described the showing as chalcopyrite-

cobalt arsenides in a westerly striking shear zone in a basic

Intrusive Nipissing diabase). The zone was traced over a length

of 500 feet. Mineralization varies in width from 9 to 25 feet and

grades of 2-3* copper and trace to 21t cobalt were returned.

Preliminary drilling (1952) showed that the mineralized zone dips

approximately 45 deg south and crosses onto the Bruce-Presto

ground ^e, Jentlna Property) at a depth of 350—400 feet.

The 1964 IP survey showed a weak conductive response over

the surface showing with much higher IP readings "over a

considerable distance to the west". The zone apparently strikes

north of west. Two drill holes south of the patent were

completed, and although assay results are not Indicated on the

-11-

drill logst Shklanka (1969) reports assays of O.70* Cu over 12.3

ft. and 1.962 Cu over 11.5 ft. Drill logs are summarized,

following:

Hole go.___Location______Bearing______Dip

5 claim SSX 68607 353 deg - 45 deg

Lithology Hineralization

O - 6.0' overburden6.0 — 22.0' calcareous siltstone

22.0 - 45.0' quartzite, bedded and nassive45.0 - 61.6' calcareous siltstone61.6 - 97.6' siltstone, argillite diss po, py at 84.0-97.6'97.6 - 99.5' quartzite99.5 - 174.5' greywacke minor po, py174.5 - 203.0' feldspathic quartzite

EOH

Hole lo. Location

6 claim SSK 69591

Lithology

Bearing

353 deg

Dip

- 45 deg

Mineral!:

O - 26.O' overburden26.0 — 40.0' quartzite40.0 - 137.0' greywacke, sheared and fractured137.0 - 193.0' greywacke, conglomerate193.0 - 383.0' greywacke cp seams at 325.0'383.0 - 404.0' chloritic shear in greywacke tr diss cp404.0 - 485.0' greywacke485.0 - 522.0* diabase

EOH

Vote that these holes did not intersect a mineralized shear

in diabase. There is no report accompanying the drill logs.

-12-

3.1.5 Canaalska Copper lines Ltd., 1965

Canamiska held a block of 42 claims covering Dobie Lake. The

northeastern portion of this block Is currently part of the

Jentlna Xain claim block (Map la). The company completed EX surveying (no report specifying method), soil geochemistry,

trenching and 4,653 feet of diamond drilling In 19 holes. A

compilation map showing exploration results Is given as Xap A.

Several EH conductors were delineated, the most significant

measuring approximately 9,600 feet ^.8 miles) long. Short soil

sample lines across the conductor returned anomalous copper-in-

solls values of up to 6,400 ppm.

Hine of the 19 drill holes were completed in the vicinity of

L32+OOB and returned significant copper values. Hole 65-11

returned an assay of 1.821 Cu over 7.5 ft. of drill core and

contains a 2.5-foot section grading 4.60* Cu. Other significant

intersections Include;

Hole l (L32+OOE, 15+10F); 0.1061 Co over 65.0* 9 110.0 - 175.O*0.2601 Cn over 7.5* C 150.0 - 157.5*

Hole 6 (L32+25E, 16+255); O.532* Cn over 25.0* 9 5.O - 30.O'2.00* Cn over 5.O* C 2O.O - 25.O*

Hole 7 (L32+25E, 16+25V); 1.441 Cn over 19.5* 9 17.5 - 3O.O*

Hole 9 (L31+75E, 16+30V); O.42* Cn over 12.5* 9 27.5 - 40.0*1.30X Cn over 2.5* 9 32.5 - 35.O*

The anomalous holes cover a strike length of 200 feet.

Geochemistry in this area returned a maximum value of 1,500

ppm and no drilling was carried out In the area of soil values In

excess of 6,000 ppm to the northeast which cover a strike length of 1,600 feet CXap A). Additionally, the coincident EX conductor

r- -is-is indicated to continue eastwards off the property. Hence, the

best part of the mineralized conductor is untested and is

apparently open to the east. This zone is on -the Jentlna claims.

Drill logs are absent from the assessment files and

orientation of strata and the mineralization may only be

surmmized from the drill sections on file. Some of the holes

apparently Intersected "greenstone" at depth, possibly Huronian

volcanics. Brief summaries of lithology and mineralization taken

from the drill sections are given in Appendix A.

3.1.6 Hanna lining Company, 1969

The company completed a 3,000-foot drill hole bearing 360

deg and with collar angle at -85 deg. Apparently part of a

uranium exploration project, the hole was located approximately

200 m east—northeast of the lo. l corner post of Jentlna Main

Group claim 1118612, north of the Little White River. The hole

intersected feldspathic quartzite to greywacke to a depth of

1,071 ft. Significantly, the remainder of the hole cut basalt,

perhaps of Archean or Aphebian age. Archean basalts are mapped

along the Little White River some 2 miles to the west, Huronian

Supergroup Dollyberry Lake Formatlorn basalts 1.5 miles to the

east (Robertson, 1969). An extensive zone of faulting was

intersected at 2,884 - 2,911 ft.; the Flack Lake Fault? Some

brecciation and shearing was also reported at 2,258 - 2,263 ft.

and plots in the vlcinty of the trace at the Little White River

-14-

Antlcllne. The log le summarized In Appendix A.

3.1.7 Paquette Claims, 1952-1965C?)

Siemiatkowska (1978) reported that two mineralized zones, a

ITorth and a South Zone, were discovered In 1952 on a 20 claim

block In the Triangle Lake area. Part of the Jentlna Triangle

Lake Group covers portions of these claims. In 1954, chip samples

across these zones assayed O.46* Cu over 3 ft. and O.08* Cu over

l ft. Some airborne geophysics was flown over the claim area In

1965. Apparently a 453-foot drill hole was completed (worker

unknown) and Intersected mainly arkose. Some minor copper

mineralization was found over a 1.3-foot width. The claim group

later became the Stanford Mines ground (Section 3.1.9).

3.1.8 Atlantic Klchfleld Co.. Triller Explorations Ltd.. 1967-68

These two uranium exploration companies held a large block

of claims in Albanel Township, probably covering most of the

Jentlna Main Claim Block. Geological mapping and surface

magnetometer surveying was carried out and was not reviewed by

the author. Two drill holes were completed; hole P-2, designated

A2 on Map la, Is situated Just north of the SE Trench (section

3.1.11 and 7.4.2). Hole P-4, shown as A4 on Map la, is located

north of Speckle Lake and close to Plcton Uranium Mines hole P4.

The holes were drilled vertically to depths of 4,587 and 2,962

feet respectively.

Hole P-4 apparently collared into diabase which ran to a

-15-

depth of 1,675 feet. This seems to contradict the drilling In

nearby Plcton Uranium Klnes hole P4 (1955) which did not

Intersect appreciable diabase. P-4 then Intersected argillite,

quartzite, arkosic quartzite and conglomerate. The hole hit thin

pyrltlc to cherty siltstone beds In an argillite unit at 1,687 -

2,350 ft. Unfortunately the drill log Is too generalized to offer

detailed structural and mineralogic Information.

Hole P-2 Intersected Interbedded argillite, chloritic

argillite, quartzite and limestone, probably of the Espanola

Formation to a depth of 4,082 ft. A section of diabase (sill)

occurs at 325 - 2,446 ft. The hole reportedly Intersected Archean

mafic-Intermediate volcanics at a depth of 4,082 ft. until the

end of the hole. Some highly sheared siltstone is also noted

within this Interval. Jo sulphide mineralization is reported.

The drill logs are summarized in Appendix A.

3.1.9 Stanford Mines Limited, 1971-1972

Blasting of a copper-stained scarp face located 300 ft.

northeast of the South Zone, Paquette Claims, (also referred to

as the Hamilton Claims and located on the current Triangle Lake

Group) uncovered a 4—6 foot wide shear zone measuring 55 ft. long

bearing 020 deg. The zone is hosted by a basic intrusive

(Stanford Xlnes, 1972) or Lorraine Formation sandstone

(Siemiatkowska, 1978). Several fractures within the shear

contained chalcopyrite filling. Disseminated chalcopyrite occurs

between fractures. Stanford reported grab sample assays of up to

-16-

7.45* Cu, 0.28 oz Ag/T in fracture-filling-type, and 1.6* Cu,

O. 15 oz Ag/T In disseminated-type mineralization. Siemiatkowska

(1978) reported quartz carbonate veining trending 265 deg

carrying chalcopyrite, malachite, azurite and specularite.

Siemiatkowska's grab samples assayed up to 15.6* Cu, 0.24* Zn,

0.36 oz Ag/T and 0.02 os Au/T. The east-west zone trends parallel

to the Bndakai Lake Fault (Map la).

Six drill holes were completed and two holes returned

anomalous copper and silver values. Hole 4 returned 0.27* Cu and

0.47 oz Ag/T over 11.0 ft. (containing a 1-foot Interval grading

1.12* Cu and 4.05 oz Ag/T) in volcanics (Nipissing Diabase?) and

hole 3 reported 0.94* Cu and 0.14 oz Ag/T over 2.2 ft. In diorite

(Nipissing Diabase?). The holes were drilled northwesterly to

intersect the 020 deg-bearing cuperlferous shear. Drill log

summaries are given In Appendix A.

3.1.10 Gowganda Silver Klnes Limited. 1972

Gowganda Silver Klnes held two large claim blocks at the

eastern end of the Jentina ground. The main Gowganda block

covered the northern part of the Jentina Main Claim Group and the

southern part of the Triangle Lake Group. A smaller claim group

covered the northeastern part of the Triangle Lake Group. The

Gowganda holdings are shown on ODK Map P.560 and indicates that

some diamond drilling may have been carried out. Other copper

occurrences, notably those on the historic Sanford Kines Property

and the patent and former patent claims at the east end of

-17-

Jentina Main Claim Block are also indicated on this map.

3.1.11 Fort Warman Explorations Incorporated, 1974-1975

The company held a block of 99 claims covering the eastern

part of the Jentlna Property, Main Block. An airborne geophysical

survey consisting of Mag, EM, radiometrlcs and resisltivity was

carried out by Barringer Research. Three areas of significant

copper mineralization were Investigated;

1) Extensive stripping, trenching and four diamond drill

holes totalling 633 ft. were carried out over the Jentina Main

Showing area (Vo. l Copper - Precious Metal Structure).

Siemiatkowska (1978) described the showing as a 100-foot long by

50-foot wide sulphide-bearing shear zone trending 065 deg and

dipping 65 deg south in silicified Espanola Formation limestone.

The shear is "rich in chlorite with minor brecciation." A 3—foot

wide zone of chlorite and magnetite-bearing limestone envelopes

the mineralization. Chalcopyrite, pyrite, malachite and azurite

were identified. The chalcopyrite occurs "as a replacement along

fractures and as massive blebs associated with quartz-carbonate

C veins/stringers] and chlorite." Siemiatkowska's three grab

samples assayed 5.352, 1.29* and 0.682 copper with traces of gold

and silver. One sample returned O.092 cobalt.

Surface plan maps of the trenches and stripped areas,

including drill hole locations are given in Figure 4.

C*46l '

-19-

The best drill Intersections are listed:

Hole 74-1: 0.99* Cu over 13 ft. at 53.0-68.0*and Included; 1.742 Cu, 0.11 oz Ag/T over 2.5 ft at 57.5-

60.0 ft. 1.35* Cu over 5.0 ft. at 63.0-68.0 ft.

* apparently a 1.9-foot section was missing In the Interval. Sludge sampling of this hole returned 1.36* Cu over 24.6 ft. at 51.0-75.6 ft.

Hole 74-2: 0.27* Cu over 3.5 ft. at 61.0-64.5 ft.

Hole 74-4: 0.52* Cu over 20 ft. at 102.5-122.5 ft. and Included; 0.70* Cu over 5.0 ft. at 109-114 ft.

Mr. Soy Rupert, the geologist on the project concluded that "the

mineralized zone....is a bedded structure interlaminated with

overlying beds and conformable with the strata " (1974), a

surprising conclusion after a review of his excellent drill logs

which provide details on lithology, structure and copper

mineralization. Copies of the logs are included as Appendix B.

2) A shear and breccia zone hosted by Gowganda Formation

conglomerate and sandstone was trenched close to the Albanel-

Vlcholas township boundary, central-east part of Jentina Block

1118696. According to Siemiatkowska, the 30-foot long trench

exposed a 10-foot wide, east-west striking quartz-carbonate vein

containing disseminated chalcopyrite and pyrite. A grab sample

assayed 2.6* copper (Siemiatkowska, 1978).

3) Some copper mineralization hosted by Espanola Formation

limestone occurs just north of Highway 546 along the Albanel-

fficholas township boundary. The 10-foot wide chlorite-epldote

shear zone trends 075 deg and dips 35 deg north and contains

-20-

narrow quartz-carbonate stringers with minor pyrite,

chalcopyrite, malachite and azurite. Siemiatkowska shows a trench

in the area (OGS Map 2399). The zone lies between the

northeastern part of Jentina Main Block and southwestern part of

the Triangle Lake Block.

3.1.12 Charles X. Mortimer. 1984

Mr. Mortimer drilled one 175-foot drill hole bearing

northeasterly near the northerly-flowing creek at the Albanel-

Micholas township boundary, now on Jentlna claim 1197740

(formerly patent claim 89P). The hole reported intersected quartz

stringers in greenstone (diabase?). to analytical results, if

any, were given.

3.1.13 International Mine Services Ltd.. 1986

This company, on behalf of A.J. Roy, carried out line-

cutting, VLF-EM surveying and reconnaissance geological mapping

on a block of 17 claims more-or-less the equivalent area to

Jentlna Block 1118612 and which includes the Main Showing. The EM

survey failed to clearly Identify the sulphide zone over the Main

Showing. Some sampling of the Main Showing was also carried out.

3.1.14 United Reef Petroleums Limited. 1988

URP optioned the A. J. Roy 17 claims and carried out

geological mapping, prospecting, magnetometer and soil

geochemical surveying using the existing 1986 grid for control.

-21-The survey provided an outcrop—geology nap with good

llthologlcal descriptions. The southern part of the property Is covered by Nipissing diabase which shows some textural zoning and differentiation.

Adjoining the diabase to the north Espanola Formation limestone/dolomite and siltstone Is napped. Soil geochemistry over this part of the property generally returned elevated copper and zinc values compared to other underlying lithologies. Mumerous rock samples also contain anomalous copper and zinc values. Although the geochemistry may imply skarn-style possibilities related to the diabase, rock samples are described as sulphide and malachite-bearing quartz-carbonate stringers / veins within limestone/slltstone with the best concentrations in a linear structural zone (the lo. l Copper-Precious Metal Structure, 1994) on-strlke with the Main Showing. The geochemical and quartz stringer zone measures approximately 3,400 feet long.

Several Cu, Au and Ag soil values were also found over Mlssissagl Formation lithologies north of the Llttel White River.

Marrow lead, zinc and gold soil geochem zones were detected In the diabase and are oriented oblique to the intrusive trend and local stratigraphy, probably delineating fault structures. Significantly, some prospecting south of the property encountered sulphide-rich quartz veins hosted by diabase. Grab samples assayed up to 1.3961 Pb, O.6581 Cu and 1,889 ppb Au (samples 4008-4011). Unfortunately, the location of these samples are not known and were not found during the 1994 project. The sample

-22-

descrlptions resemble those from the Vhlte River Lead Mine

(section 3.1.1).

Channel sampling of the Main Showing came up with 5.35*

copper over 23 ft. from the main pit (Pit 1); this sample

interval contained a 13—foot section which assayed 8.981 copper

and O.020 oz gold/ton. A pit situated 10-20 feet to the east of

Pit l returned a channel sample value of 0.8421 copper over 6.6

feet.

Sock sample descriptions and assay results of anomalous

samples from 1988 are given in Appendix C. Most of the samples

are indicated on Map l, HV Sheet, Geology and Mineralized

Structures.

The magnetic survey shows sparse contrast, perhaps a

function of wide line spacing (400 feet) rather than lack of

variation In magnetic signature across the property.

3.2 Academic and Government Studies

3.2.1 Paul Schecrer, University of Wisconsin, 1956

Mr. Scheerer carried out geological mapping at a scale of

4" sl mile in the Albanel-Vicolas townships area. The study

outlined the geological units In the Jentlna Mine property area

and identified a substantial fault structure along the northern

ridge of the Little Vhite River valley. Part of this structure

may be a portion of the Flack Lake Fault.

-23-

3.2.2 J.W. Gash and T.A. Vogel, University of Wisconsin, 1959

These two researchers napped approximately the sane area as

Scheerer. An east-west antiformal structure was mapped across the

northern part of the current Jentlna Main Claim Block in Bruce

(Espanola?) Formation limestone. A northeasterly anticlinal-

synclinal pair is noted within Gowganda Formation sediments Just

north of Le Scarbo Lake.

3.2.3 Provincial Government Surveys

Geological surveying of Vicholas Township was carried out by

the Ontario Division of Xlnes in 1969 at a scale of 1:31,680, ODK

Map 2347 (Robertson, 1969). The mapping also Included Raimbault

Township which adjoins nicholas to the east. There Is no

accompanying report. Albanel Township was mapped at the same

scale in 1974 by K. X. Siemiatkowska and Includes west adjacent

township Varley (OGS Map 2399). OGS Report 178, "Geology of the

Endikai Lake Area", 1978, accompanies the maps.

3.2.4 Federal Government Surveys

The Jentlna property areas are covered by l" = l mile

Geological Survey of Canada aeromagnetic maps Flack Lake — Map

2241 G and Wakomata Lake - Map 2227G (1962-1963). The survey

shows a prominent circular magnetic low feature over the Main

Showing area on the Jentina Property. The magnetic data was later

digitized by the OGS in 1993. Figure 5 Is an MR&J computer

printout of the digitized data covering the Jentlna claims.

-24-

Figure 5: Regional total field magnetics

Figure 5: Regional total field •agnetics covering tie Jentli

-24A-

Results of a regional lake geochemical survey was published

by the GSC In 1987. An anomalous copper value of 980 ppm is

reported from Triangle Lake. Significantly, the trace of the

east-west striking Endakal Lake Fault crosses the lake OCap Ib).

-25-

4.0 KHGIOWAL GEOLOGY AID XIIEBALIZATIOI

4.1 Geological and Structural Framework

The Jentina Mine Property is located at the north-central

part of the Huronian "Basin" of Proterozoic-aged Huronian Group

of mainly fluvial, in part glacial, clastic sediments and basal

tholeiitic to alkaline volcanics (Roscoe and Card, 1992, Bennett

et al, 1991) (Figures 6 47). The region of Huronian

sedimentation, extending 145 miles from Just east of Sudbury to

Sault Ste. Marie to the west is designated the Southern

Structural Province.

The Basin is considered to have been a passive rift during

Archean times, activated circa 2.4 Ga with the uplift of

surrounding Archean blocks, contemporaneous extrusion of volcanic

rocks and subsequent deposition of the Hough Lake, Quirke Lake

and Cobalt groups circa 2.45 - 2.2 Ga (Bennett et al, 1991).

Provenance of the sedimentary material is indicated to be from

the northwest (Bennett et al, 1991, Roscoe and Card, 1992)).

The essentially east-west curvilinear Flack Lake - Endikai

Lake Fault System, which crosses the northern part of the Jentina

claims, defines the unconformity of Huronian sediments to the

south with Archean volcanics, granites and mlgnatltes to the

north. The Flack Lake Fault, traced over a distance of 150 Km

(Siemiatkowska, 1978), is considered to be a reverse thrust

fault, probably a prior, Archean—aged normal fault, which was

reactivated during the Penokean Orogeny circa 1.8 Ga (Bennett et

al, 1991 and Fyon et al, 1992), probably not unlike other

rtU

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-28-

lum rift

MdCm l Rift crus?

Fy.:g Cocctt Group

l |Qurt* LfiM Group

Cntk Usmc normal

Figure 8: Schematic diagram Illustrating the paleotectonic aodel proposed for the feu nation and deformation of the Huronian Basin (after Bennett et al. 1991)

-29-

regianal Archean boundary faults, for example the Cadillac Break

in Quebec. The Cadillac Tectonic Zone separates Early and Kiddle

Archean supracrustals from Late Archean basinal sediments, the

Timiskaming Group ( Hubert et al, 1984, Gauthier et al, 1990,

Villoughby, 1993). A continental-arc collision

mechanism Is envisioned to have been operative during Penokean

deformation by many researchers (Figure 8) (Bennett et al, 1991).

Locally, the Flack Lake Fault has produced considerable ductile

shearing and brittle deformation of host rocks with attendent

brecciation and quartz veining (Anthony and Villoughby, 1988).

Numerous northeasterly and northwesterly faults are also

delineated and as a reponse to various degrees of movement along

all faults a series of fault-bounded rotated blocks were formed.

Many llthologlcal contacts may in fact be tectonic (Villoughby,

this study).

The Penokean deformation features (folding, faulting)

affected both Archean and Huronian rocks and Indicates general

north-south compression and may be part of the postulated Great

Lakes Tectonic Zone stretching from Sudbury west to Minnesota

(Bennett et al, 1991).

Intrusion of Vipissing diabase and gabbro sills are dated at

approximately 2.2 Ga, prior to the main deformation event. These

intrusive bodies occur as undulating sheets and/or funnel—shaped

bodies intruding both the Archean basement and the Hurionlan

sequences.

A tectonic chronology and timing of metallogenic events,

-29A-

irlzed by Fyon et al ^992) is given as Figure 9.

The geology In the area of the Jentina Property la given In

Haps la, Albanel Twp and Ib, Nicholas Twp. A local table of

formations is listed, Table 1.

'!3

aiitl

332393333

• ••l ill li

—

m

1 M

'

i \

jjiii 1,1

111 liii it liijif.

i81

j ——

— i.

nalH

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40.—

J

iii liiiiiil Ih

M.,

1——

1 II

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1

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C

Table 1: Table of For aa 11

attddle precanibrian 13 Vlplsslng Diabase, Gabbro

ELLIOT LAKE GHOUP

12 Dollyberry Lake F- andeslte/basalt

COBALT 6BOUP

11 Bar River Formation — orthoquartzite

10 Gordon Lake Formationand si l t st

Lorrain ForvatIonconglomerate

8 Gowganda Formation— mainly conglomerate, arkose, feldspathic sandstone and siltstone

QUIHKE LAKE GSODP

7 Serpent Formation— feldspathic sandstone, arkose, calcareous

sandstone, minor siltstone, conglomerate

la Fomntlon- limestone, dolomite, calcareans- calcareaaB sandstone, siltstone

Broce For matIon Le

BOUGH LAKE GBODPKlsslssagl Foraatlon

— feldspatnlc sandstone

Granitic Intrusive Bocks- nonzonlte, granodiorite, trondnjealte

Gneissic Intrusive and KLgaatltlc- orthognelss, ndgnwtlte, amphibolite

rtavolcanlc and netasedlaentaryTlc—felsic volcanics, minor sediments

-32-

4.2 Base Mietal and Precious Setal Production

Over 120 copper and polymetallic and /or precious metals occurrences are docuaented within the Huronian Basin. Documented production is 183,787,631 Ibs copper, 91,027 oz gold and 146,321 oz silver, representing a value of S219,768,309 (copper at S1.16/1b - Globe A Mail, Sept 1/94; gold at 3386.90/oz - Globe ft Mail, Sept 2/94; silver at 35.21/oz - Northern Miner, Aug 29/94). Most of this recorded production was returned from the Pater Mine which yielded 78,694,117 Ibs copper, 4,613 oz gold and 139,509 oz silver and Bruce Mines which extracted 95,186,000 Ibs copper. A list of area production is given as Table 2.

Current copper Inventory alone in currently non-producing developed mines stand at 73,964,000 Ibs valued at 885,798,240. The Bi-ore Mine alone has reserves of 400,000 tons grading 4Z copper or 32,000,000 Ibs of copper. Current reserves are listed in Table 3. There is no data on precious metals content, however

st of the copper producers also report gold recovery.

-33-

iaDJ.e A \ ijisi ox trapper m rreciouB Jtei.aj.s n-oancxion in XJie Southern Province (excluding tie Sudbury Basin and Keweenawan deposits)

KIBE COPPER Ibs

Long Lake Eden Twp

VorstarDavis Twp

KcKlllanKongo win Twp

Bousquet Curtin Twp

PaterSpragge Twp 78,

Shakespeare Shakespeare Twp

HavilahGailbrath Twp

BaldwinBaldwin Twp 3,

HermlnaSalter Twp 1,

Massey Salter Twp

Bar FinThompson Twp

Bruce XinesPlummer Ad Twp

Bruce-PrestoPlummer Ad Twp

Cheney Gould Twp

GouldGould Twp

Bi-OreSagard Twp 1,

Glagona Gladstone Twp

Rock LakeAberdeen Twp 1,

Dona IdaXaasey Twp

XcKeeOtter Twp

995,594

694,117

525,842

015,950

2.5*

120,000

95,186,000

1.59%

400, OOO

647,079

1,785

524,000

633,264 (4.51)44,000

GOLD oz

(0.26) 56,742

10,600

10,593

4,655

4.613

2,447

1,030

347

SILVER oz TOHVAGE

674 221,070

39,100

378 60,139

196 17,393

139,509 2,292,506

8,599

214 6,589

5,350 146,316

13.134

14,750

1,500

300, 000

139

33,468

7

2,726

28.2

43,300

500

Total: 183.787,631 91,027 146,321 3,201,257

-34-

Table 3: Documented Copper Inventory in the Huronian Basin

Mine Tonnage Grade Calculated Copper InventoryBald Done 405,600 0.25* 1,014 TBi-Ore 400,000 4.00* 16,000 TMaster 162,787 1.73* 2,816 TCannon 160,000 2.03* 3,248 TBoyea 128,000 1.93* 2,470 TAbbican 105,750 1.08* 1,142 TBilton 95,160 1.72* 1,637 TPrinciple 86,386 2.26* 1,952 TTwin Lakes 76,900 1.73* 1,330 TCopper Prince 50,000 3.00* 1,500 TStelnberg 47,000 1.82* 855 TBruce 40,000 1.80* 720 TCheney 39,404 3.97* 1,564 TCambell Dukes 33,000 1.20* 396 TBruce-Presto 13,500 2.50* 338 T

Total——————1,842,887 36,982 T——

r

-35-

4.3 Mineral Deposits

Earlier reseachers, notably Pearson (1978, 1979) and Innes and Colvine (1990), have Identified and classified the various styles and patterns of base and precious metal occurrences of the Huronian Basin. Pearson studied specifically copper metallogeny of the Huronian, however many of the copper deposits contain other base metals and precious metals and are probably best described as polymetallic (Table 4, Figures 6 ft 10-12).

Review of various literature providing deposit descriptions and some property visits by FR4J personnel over the past 6 years, indicate that most deposits in the region are structurally controlled, sulphide-bearing quartz vein or breccia/alteration zones (chlorite, silica, carbonate, albite), or mineralizaed breccia pipes. Most contain significant magnetite, hematite and specularite. Pearson's classification, aside from "veins", apparently relies on host rock type such that mineralized veins in Huronian volcanics are VMS deposits, those in Lorrain - Gordan Lake Formation sandstones are SEDEX deposits, deposits hosted by Espanola Formation limestone close to diabase are skarn deposits, etc. Brief descriptlions of selected deposits are given by way of illustration.

The Pater Hine consisted of two, 1,000-foot long by 7-foot wide ore shoots in a shear zone hosted by schistose Huronain metasedlments and metavolcanlcs. The deposit was delineated to a depth of 4,000 feet. Mineralization consisted of chalcopyrite, pyrrhotite and pyrite in brecciated quartz veins. Copper grades

-36-

averaged 2. Q71L. The shear structure runs oblique to the Hurray

Fault. The deposit is probably not VMS-style.

Auriferous, arsenopyrite—rich quartz veins at HcXlllan are

localized along a drag fold within Gowganda Fornation quartzite

at the contact with nipissing diabase. The main vein measured 25

feet wide over a strike length of 300 feet to a depth of 325

feet. The style of mineralization is considered typical of the Au

+S- Cu -bearing vein catagory. Gold grades averaging 0.18 oz Au/T

were mined. The main vein measured 30O feet long by 25 feet wide

to the 325-foot level.

At Bi—Ore, average grade of ore milled was 4.0* copper. The

deposit Is described as a series of fissure veins lying along

faults in host cherty quartzite. A property visit by IB&J in 1993

found chalcopyrite mineralization In albitlzed material.

Both the Scadding and Long Lake mines are mineralized

breccia pipes. The Long Lake body measures 250 feet long by 250

feet wide, plunging steeply southeasterly to a depth of 340 feet.

Mineralogy consisted of pyrite, arsenopyrite, pyrrhotite,

chalcopyrite and galena. Mill-head grade at Scadding was

reported as O.159 oz Au/T.

Although some skarn—type deposits occur in the region may be

related to nipissing intrusion (2.2 Ga), most vein-type deposits

post-date intrusion at 1.8 Ga, probably hydrothermally /

epithermally generated during Penokean Orogeny (Fyon et al,

1992). The Vo. l Copper-Precious Metal Structure on the Jentlna

Property, although hosted by Espanola Formation limestone/

r-37-

siltstone close to diabase, snows no contact metasomatic features. A description of the Foster occurrence by Pearson (1979) reports tungstun, molybdenum, copper, zinc and silver in idocrase dlopslde-garnet skarn In Espanola Formation rocks, adjacent to a diabase sill.

Both Pearson (1979) and Chandler (1984) report on possible red bed copper mineralization at Stag Lake and Cobre Lake, 20 miles east of the Jentlna Property. The mineralization consists of disseminated chalcopyrite and pyrite localized along the contact of Lorrain Formation arenite with Gordon Lake Formation mudstone/sandstone. Vo significant copper concentrations are as yet reported, however the contact is mapped over a length of 3.2 Em. Currently, the Ontario Geological Survey is investigating red bed copper potential of this area (Hike Hailstone, Assisstent Regional Geologist, Sault Ste. Marie,; personel communication, July, 1994).

Ho significant Vi Cu mineralization Is reported in the central and western part of Southern Province.

The Coppercorp and Tribag deposits (Hellkean-age) at Mamainse Point, north of Sault Ste Marie, catagorlzed as porphyry by Pearson, are generally considered to be breccia pipe mineralization Clorman and Sawkins, 1985 and Richards and Spooner, 1989). Some breccia-like orebodles are recognized In the Huronian, eg Long Lake.

Many of the vein and breccia-type deposits are accompanied by soda metasomatism or albitization (including Jentlna). Fyon et

-38-

al (1992) describe the nature of albite alteration, quoting

various sources, notably VIIf Meyer of the Ontario Geological

Survey: "the alteration is manifested by veins, dike-like zones,

stratabound, areally extensive massive zones and zones of

brecciated, altered rock". At some gold deposits, eg Scadding,

albite is commonly replaced by carbonate and later quartz-

chlorlte. Commonly associated with Sudbury Breccia and Sudbury

area Huronian rocks, albitization is dated to 1.7 Ga (Schandl,

1992 and Fyon et al, 1992), implying that at least the Au-Cu vein

association is younger than the formation of polymetallic veins

(1.8 Ga, deposited during the Penokean Orogeny, Figure 9).

Schandl points out that the presence of albite may relate to

"deep—seated plutonism and faulting". Perhaps the presence of

albite is a necessary signature of polymetallic deposits rich in

gold.

As yet, no Archean—style lode gold deposits have been

discovered, however the tectonic setting of the regional Flack

Lake Fault Zone bears some similarity to the Larder Lake—Cadillac

Tectonic Zone, Abitibi Belt, which historically hosts numerous

commercial gold deposits (Gauthier et al, 1990, Willoughby,

1993).

-39-

Table 4: Classification of Copper Deposits for tile Huronian. Basin (after Pearson. 1978. 1979)

Yein—type:

dialcopyrite—pyrite-specnlarlte veins;Crownbridge, Bl-Ore mil

b. polymetallic - Zn— Pb-Ag-Cn; Jardnn- Pb-Ag-Cu; Prace- Cn Cbornlte—cnalcocite— native copper;

Co- Cu-Co- (Bi-U-Mi); Bnrdon Lake

An- (Cn)— bearing veins; Shakespeare, XcKlllan

2. Contact MetaeoMatic (Skarn)—type:— Cobden Kiver, Desbarats Lake. Foster

3. Cu-Wi in mafle—nltravfic intrusions

4. SEDBZ- Stag Lake

5. VBS and stringer- Pater

O*— Tribag, Jorgan (Xeweenawan)

-40-

Flgnre 10: Copper deposits at Pearson. 1979)

Southern Province Cafter

-41-

*——~H• d* BM

Figure 11: Gold and polymetallic m± lin Cafter Fyon et al.

il depo8l*ts In the Huronian 1992)

ra H- tt

l L 5!o H m H

tr H-

"

4

l!

Jla l

l (O

r* -43-5. O EZPLOHATIOV MODEL

5.l Polymetallic Veins, Breccias and Breccia Pipes

Any exploration model for this portion of the Huronian

Supergroup must account for the variation In quartz vein and, In

particular, breccia morphology. Excellent reviews of breccia

morphology and origin are presented by Laznlcka ^988) and

provide several mechanisms of breccia formation Which may fit the

observations of mineralized veins/breccias In the Huronian.

Figures 13-15 show various breccia vein and breccia types and

offer some Insight Into mechanism of formation, for example,

high—angle faults to Intersecting faults as tight, narrow zones

at the mesoscopic scale to collapse breccias at the macroscopic

scale to "blow-outs" related to Intrusive or gaseous deep—seated

plutonism. All of these features provide potential traps for

epithermally generated metal-bearing fluids. An end member may be

the emplacement of a diatreme with morphology and mineral

distribution as shown in Figure 16.

Atkinson et al (1982) report on breccias formed in sediments

adjacent to intrusive rock bodies at the Victoria Mine, Mevada.

The term skarn-breccia is widely used (Figures 17 A 18).

Useful models of mineralization in breccia pipes hosted by

Proterozoic volcanics and sediments are provided by Olympic Dam,

Australia (Figure 19) and Vernecke Mountains, Yukon (Figure 20),

respectively. Several deposits are known in the Olympic Dam

region and combined reserves are 2 billion tonnes grading 35* Fe,

1.6* Cu and 0.05* U3O8 (Hitzman et al, 1992). Vernecke Mbuntan

-44-breccias host l million tonnes containing 297* Fe plus 500,000 tonnes of 0.571 Cu (Hitzman et al, 1992).

Hltzman et al suggest that this style of deposit Is "a distinct class of ore deposit characterized by low-titanium, iron-rich rocks formed in extensional tectonic environments", for example, at continental margins and subduction zones (Figure 21). Such a geological environment has been postulated for the Southern Province (Bennett et al, 1992).

Given the current state of knowledge of Huronian Supergroup mineralization, this style of mineralization is considered the main target for economic mineralization at this time.

C996I 'vatofuxf^

x r C -* v v~W/ -'--^^'^w-v/i^4-;"J5- - f - i v

-9*-

-46-

16-16. tiaaalM *f (early Tertiary Pb-Zn-A*J Crm tbm•t al. (1908). (1) Irootbergtraaelclm becvem a wo* of Datcad: el^ |oaM M!*M*- (2)•awcBut; b-eaab qnarcz border MM; e-pyrtt*;•llleiflcd gmlM riBialil lin tb*

. by Fmraavtc

Colorado Froat ai graaita aad

Vela.

grmiUe (*)

ta bneelatloa d•phalarlt*; ,

(3) TmUcmn Vt&n. aptalwit*Co braeeliccd almklta putpUyrj dike Chat latrudiJ mltmrmt fUa. mbaUrlO f mint Ing fmlc rabble la gmiM. (3) or a mbalnlta vvia (dark), bneetctlon of tb* loot •luklto •C Cnffamto by otdorito (dot*). (6) ••rrlna lodo (apmluit*. dark), faulead. braeclaud md eat by a ynnaaar vyrlto mia. (7) Tola (aphalarlta. pyrite, ealeaa)

16-12. Imlc eattlag laterbaddad breccia only vhm It la

(ItSO). •rerbmrldga. Colarado.dllatea aad fill*

Crm Ltmrlat aad

Figure 14: Fault breccia developaen-t governed by rock (after Laznlcka, 1968)

•ney

-47-

veu

16-10. Variety of fraecuna aad faolta ia brittle rocka aaaoeiacod wich breccia*, •ac to acale. (1) "Typical' dllattnual oonal fault; (A) crackle breccia ia valla; U) friorf.- f COB valla, little -~"*l'rJ; (CI drafted, abraded, rotated fraaucau. (D) "borae". (2) Caapoalte fault (Multiple fault cone); aatt-dUacioaal to jn\*rmQ allp plaoaa (E) alternate with dilated, breccia-filled oaoe (F). The no* la ailiciflad and fane e bold outcrop; (G) Injection of breccia into vallncka. (1) ne* uich rotated aad partly allied fraceenta ia the centre (H), gradlnc lato crackle breed* la the valla (I). (4) Ulecaat flaaure gravity-filled by rubble U) and froB the valla (K). 15) Crouch fault with fill (L) andatleaal OD. (6) MB-diUciaaal flight) fault represented by e thin allp plea* (7) fleeure breccia vela. Tram l-arairka CI9V7}

Figure 15: Breccia 11 (after L rlcka.

doe to faulting and. fractiirlng 1988)

-48-

'fS\ U(V) . surficial solutions

wallrocks formation

Au-Ag(Pb.Za.Cu)

fluids from depth

orebody la wallrocks (magnetite)

supergene development

nCDBE ft-*. TlBlat oC orltln of tbm *Lfh 'tor cjpoa of Mcallle Blaar&lluclao la

Figure 16: Karphalagy of a diatreme sbowlng relative sites of possible Mineralization Cafter Laznlcfca. 1988)

-49-

Figure 17: Morphology of mineral ized breccia in host sedlaents at the Victoria Mine, levada (after Atkinson et al. 1982)

-50-

A'

E

Frc.1 Sectta A-AM Ae pipe hat rotated 30T to the e-Jt i

Figure 18: Klaerallzed (after Atkl

•tt-breccla at the Victoria Mine, et al. 1982)

-51-

Boct-ore

1km. t

OLYMPIC DAM BRECCIA COMPLEXSignificant occunenoes of hehsuliiic granitic

breccias hxally with hematite-rich matrix

Caiidner dikes and Beda volcanics - dolerite and mafic volcanic racks Panduia Formation - nad beds Gawlernnge volcanic rocksHil

Lincoln Complex : defanned granitoids: syntectonic (Kiinban)

Figure 19: Schematic diagram of the form and structure of the Olympic Dam and Acropolis deposits, Australia after Hltzman et al, 1991)

-52-

POTASSIC/ SERICITIC ALTERATIONi i DKBchcd md fractured 1——'rock

^3-Skarn'

•l Hematite g|3| Caibonate-diJorite- ^^^ (magnetiteMhematite) E7TS Sericile-ehlorite-

SODIC ALTERATION CJ Magnetite

Albile-scriciteH urtite

l ABrite-Onagnetite)

20: Schematic diagram showing for; of the sedimentary-hasted deposits (after Hitzaan et al.

and alteration featiXbnntain—type Cu-Fe

1992)

-53-

OLYMFIC WERNECKE BAYAN DAM REDBANK OBO

KIRUNA GREAT BEAR&E MISSOURI MAGMATIC

ACROPOLIS ZONE

Figure 21: Tectonic setting at Olympic DaB-Vernecke ftrantain.breccia style precious and base aetal deposits Cafter HitzBon et al. 1992)

-54-

5.2 Volcanogenic massive Suphlde Deposits

Although no significant VMS deposit has been discovered in the volcanic rocks of the Huronian Supergroup, naselve sulphide deposits are important in the FIin FIon-Snow Lake district of Aphebian volcanics, northern Manitoba (Figure 22). The Anderson Lake Klne (Figure 23) had reserves of 3.3 million tonnes grading 3.44* Cu and O. IX Zn in 1977 and the FI in Flon Klne reported reserves of 62 million tonnes grading 2.18Z Cu and 4. tt Zn In 1977 CValfrod and Franklin, 1982). A VMS deposit model is considered to be viable for the Huronian Basin.

Additionally, an Archean VMS deposit may lie buried at depth beneath the Huronian supracrustals. Archean volcanics are Indicated to outcrop Just to the north of the Jentina Milne Property.

5.3 Archean Lode Gold Deposits

The Flack Lake Fault Zone is considered to represent a regional unconformity between Huronian supracrustals to the south with Archean "basement" to the north and indeed may be the northern boundary fault of the Huronian Basin. In the Jentina Property area, the fault zone comprises several fault traces containing some sizeable wedges of Archean granitic and supracrustal material.

The geological literature is volumous with descriptions of quartz vein-hosted gold deposits localized within brittle-ductile deformation zones which are generally formed along the trace of

-55-

these aajor regional unconformities or "breaks", for example the

Cadillac Break In Quebec. Deposits are frequently found in

subsidiary structures to the "breaks" within the older Archean

volcano-sedimentary sequences as well as within the younger, Late

Archean sedimentary basins, the Timiskamlng-type sediments. The

sediments represent baslnal fill material from the uplifted

Archean sequences.

The Huronian sediments and volcanics represent in-filling of

a rift system with material mainly derived from the Archean

hinterland to the northwest. Although no lode gold deposits have

been Identified, the Archean-Proterozclc interface, particularly

in the region of the boundary faults, may provide gold targets.

5.4 Exploration Teclmlqi

In general, surface EX geophysical methods are ineffective

in the delineation of the relatively narrow mineralization

(averaging 10 - 25 feet) and erratically distributed sulphides

within polymetallic structural zones. Part of the problem has

been the configuration of geophysical control grids. To

geophysically explore for the high grade ore shoots prevalent

within these narrow, however extremely long structures (in some

cases greater than one mile), line spacings of 100 feet or less

are necessary, with stations of less than 25 feet. Magnetic

surveying also will benefit from detailed griding as narrow,

enveloping iron-rich alteration packages (chlorite, magnetite)

associated with

-56-

minerallzation, will be read.

Soil geochemistry has been shown to be successful in

cases, for example the Canamlska work in the southwest part of the Jentlna Property.

To the author's knowledge, no detailed structural napping has been carried out In the north—central part of the Huronian Basin. The Jentlna napping Identified at least two orders of schistosity plus countless fracture, cleavage and minor fault orientations. Undoubtedly, unknown structural domains await discovery, some of which may contain economic mineral concentrations.

Jo systematic mapping and rock geochemistry over many of the area showings has been tried or documented. Happing, together with magnetic surveying and aerial photography are considered the best methods of delineation of structures and pipe-like features. Mechanical stripping of the extension of known mineralized zones is also a good prospecting tool.

-57-

ri Moore(HW). Unit moen

NA - NorAcme (cold). S - StaL L*- Linda. R - Rod.A-DHt-

•s follows: H - Ham Lake Stack. O - Grassy River Stock. HB - HtaUet i. P " Pidver Gneiss Dome. W ™ Wckasko Slock.

Figure 22: Protei le volcanic-hosted TB5 deposits In the Snow Banltoba Cal-ter Waif ord and

Franklin. 1982)

-5a-

Figure 23: Section at the T1S line, Manitoba (afterValford and Franklin, 1982)

-59-

6.0 GEOLOGICAL IAPPI1G AID SAHPH1G PKOGRAM

A two phase program of lisostructural napping, blasting X trenching and systematic sampling was carried over two stunner field seasons in 1993 and 1994.

The 1993 (June) portion of the program consisted of 76,550

feet (15 miles) of linecutting covering claims 1118612 and 1113613 and prospecting along the strike of the known copper- silver-bearing, structure (the Kaln Showing) located in the northeastern part of claim 1118612 (L31+OOE, 16+005), Albanel Township. Claim 1118612 is the main portion of the original Art Roy 17 claim block (1986-88).

Most of the linecutting was carried out on 1118613. A tie line at 10+OOV was cut across 1118612 and some short cross lines were cleared, more-or—less corresponding to the 1986 control grid. The tie line follows the trace of the lo. l Coppez—Precious Metal Structure. The original baseline was re-cut from LO+00 west

to L24+OOY and extended to L44+OOY over claim 1197219. Line spacing is 40O feet with stations every 100 feet.

A program of blasting and trenching was carried out in mid-

July over various parts of the Vo. l Structure in the area of TL10+OOF. The pit at the Main Showing was also cleared out and re-blasted. A total of 22 rock samples were collected, both grab and chip channel. ICP analysis (32 elements) was carried out by Chemex Labs Ltd., Klsslssauga, Ontario.

A 400-foot spaced line grid totalling 124,430 feet (23.6

-60-

rniles) was cut In Hay and June, 1994 over the southern claim area

(excluding southwestern claim 1186889). From mid-June to mid-July lisostructural mapping, prospecting and sampling was carried out over most of the grid area, including the 1993 grid. Claim

1118696 nicholas Township, which was grided in 1994 was not

investigated at this time.

Happing was carried out at a scale of l" = 100' using the

cut grid, topographic maps and alrphotos for control. The final

geology and mineralized structure maps are presented at a scale of l" - 200' in four sheets (FV Sheet, SV Sheet, IE Sheet and SE

Sheet). Topographic bases were produced from a digital

computation compiled by BR&J, printed by The Drafting Clinic, Kissassauga, Ontario. Drafting services were performed by Xlnroc

Management Limited, Toronto and 9R&J Resource Associates Limited.

A total of 45 rock samples was collected, many chip channels, and assayed for copper, gold and silver at Chenez Labs, Kississaugua, Ontario.

Art Roy, the property holder, subaitted 4 rock samples from

Trench l (the lo. l Structure) to Royal Oak Mines Inc. of

Timmins. The company assayed the samples for gold and also

performed some multi-element analyses.

The Triangle Lake claims north of the Little Vhlte River and claim 1186889, Dobie Lake, which adjoins the southwestern part of the main block, were not visited during the course of the 1993—94 project. Assessment data for these areas however are reviewed in this report (section 3.0).

-61-

Llnecutting was carried out by fform KcBride, Votre Dane de

Ford, Quebec.

Personnel: Mr. Art Roy retained the services of VR&J Resource

Associates Limited of Toronto, Ontario to carry out the program.

Lithostructural mapping and Interpretation <1994> was carried out

by H. O. Willoughby, B.Se. (Bans.), President of IR&J Resource

Associates Limited. Mr. Willoughby was assisted by Chris

Marchildon, Pe ne tang, Ontario, a. recent graduate from Sir Sanfred

Fleming College. Mr. Marchildon carried out prospecting, grab and

channel sampling plus some geological mapping. J.M. Sirunias,

H.A.Se., P.Eng., Vice President - Engineering of FR&J Resource

Associates Limited, Kississauga, Ontario, directed the 1993

trenching/blasting and sampling program.

-62-

7.0 EXPLORATION RESULTS

7.1 Preamble

The field study was designed to Investigate the nature and

extent of the various known copper and precious metal-bearing

structures as well as other, previously unrecognized, local

structural features faults, shears, folds). Detailed lithologic

and stratigraphic analysis was not attempted and lithologlcal

designations generally conform to those established by government

surveys (see Siemiatkowska, 1978 and Robertson, 1969). However,

It was possible to subdivide the Gowganda and Espanola formations

at the property scale during the course of systematic grid

mapping.

Vumerous fault and airphoto lineaments, not previously

mapped or recognized by the OGS, are important contributions to

the knowledge of the geology in the general Endakal Lake area and

on the property. Some are considered by the author to have played

a significant role in the distribution of mineralization on the

Jentina claim block.

7.2 Geology and Distribution of Llthological Units

The study area is dominated by a high ridge of nipissing

diabase stretching east-west across the central part of the claim

block from Le Scarbo Lake in the west to and beyond the property

boundary in the east. An irregular mass of diabase occurs along

the east shore of Le Scarbo Lake on the Falconbridge patent and

to the southeast onto the Jentina property. Some vertical cliff

-63-

faces are presented CPlate 1).

Espanola Formation llmestone/dolomite and siltstone envelope

the diabase, with limestone the matin lithology to the north,

siltstone to the south. The Espanola encloses the western end of

the diabase and folding (synformal) is evident. The fold axis may

be occupied by the diabase sill, however bedding features south

of the Intrusive are Indicated to dip and young (rhythymic

bedding) to the south conforming to the southerly dips of

Espanola Formation limestone/siltstone north of the diabase. In

general, bedding is shallower north of the sill.

Bb contact metamorphic features contact are evident, however

limestone is contorted and brecciated close to diabase.

Espanola Formation lithologies north of the diabase host the

Fa. l Ccpper-Precious Metal Structure, while part of the Ha. 2

Copper Structure, located south of the diabase, Is hosted by

Espanola Formation siltstone.

StratIgraphically underlying the Espanola Formation, and

north of the diabase sill, are a few exposures of Bruce Formation

conglomerate and greywacke. Exposures of older Misslssagl

Formation feldspathic sandstone occur along the steep northern

slope south of the Little Vhlte Elver and along the northern

course of the river (Plates 6 and 7).

Gordon Late Formation sandstone is indicated to outcrop

along the Little Vhlte River at the northwestern part of the

claim block. The trace of the Flack Lake Fault trends east-

northeasterly across this part of the property. The author did

-64-

Table of Formations

9 Viplssing Diabase, Gabbro— undlfferentlated

HUROVIAV SUPERGROUP

COBALT GROUP

8 Bar River Formation— light grey quartzite, massive—bedded, ripple marks

7 Gordon Lake Formation— buff-pink Interbedded sandstone and siltstone

6 Lorrain Formation— hematltic pebbly sandstone, conglomerate

(not represented in 1994 survey area)

5 Gowganda Formation— d. reddish arkosic sandstone—c. red—pink granite and arkose pebble—cobble

conglomerate— b. grey—grey green siltstone, quartz-rich

(quartzitic) siltstone—a. grey heterolithic conglomerate

QUIRKE LAKE GROUP

4 Serpent Formation— pinkish to light grey—green feldspathic

quartzite

3 Espanola Formation— b. clastic sediments; mainly grey—grey green

siltstone with some quartzitic, calcareous siltstone/sandstone

— a. non—clastic sediments; mainly brownweathered limestone with some dolomite and cherty horizons; generally laminated with thin siltstone laminations.

2 Bruce Formation— greenish grey polymictic conglomerate,

greywacke

BOUGH LAKE GROUP

l Xisslssagi, Formation— pink—green feldspathic sandstone, ar!

-65-

not visit exposures of Bruce, Xlssissagi and Gordon Lake

formations during this program. Outcrop locations are taken from

the 1988 United Beef Petroleums mapping.

The western and southern part of the property is dominated

by conglomerates, quartzltes and siltstones, quartzitic

slltstones assigned to the Gowganda Formation (Plates 2-4). The

mapping identified four units within the Gowganda and are listed

and descibed in the Table of Formations. The sandstones and

conglomerates are fairly massive and some of the numerous Joint

measurements may represent bedding. Some graded bedding in the

arkosic sandstone member was recognized, for example L12+OOY,

2+75S (Plate 5). An example of Gowganda Formation heterolithic

conglomerate is shown in Plate 9. Quartz veining and chloritic

shearing in Gowganda Formation polymictic conglomerate close to

the Albanel-fficholas township boundary is Indicated to be part of

the Ho. 2 Copper Structure.

Difficulty was encountered distinguishing Serpent For-™**"**

feldspathic quartzite from Gowganda Formation arkosic sandstone.

Serpent Formation outcrops at the western end of the property

along Highway 546 and a small, probably fault-bound section

occurs south of the diabase sill centred at approximately

L48+OOV, 4+OOS. Quartz veining and stockwork In this area may be

the western extension of the Ho. 2 Copper Structure.

An extremely high ridge of grey, ripple-marked quartzite in

the area of L20+OOV, TLIO+OOH Is probably Bar River Formation

(Plate 5). Previously the exposure was Included within the

-66-

Espanola Formation (Siemiatkowska, 1978 and Anthony and Willoughby, 1988). The outcrop gives a good view of the general terrain on the property (Plate 6).

7.3 Structural Geology and Mineralization

The lithologles display a pronounced east-west structural trend as indicated by bedding, schistosity and (fracture) cleavage plus shearing. For the most part schistosity or cleavage (SI) dip steeply to the north with bedding (So) mainly moderately to shallowly south dipping. Some rare 2nd order cleavage (S2) was noted. The author suggests detailed structural measurements and analysis are necessary to determine the significance of many of these features. Possibly another phase of folding other than that Indicated from bedding, may be deduced or structural domains relating to mineralization may be outlined.

Extensive shearing is associated with the Id. l and lo. 2 Copper Structures. These predominately chloritic zones dip very steeply to the north.

Several northerly fault traces are evident from field mapping and airphoto studies (Haps la, Ib, geology maps). The fault running through Le Scarbo Lake terminates the main portion of the diabase sill as well as cuts off the western extension of the Ho. l Copper-Precious Metal Structure (Geology Map, BY Sheet). A grab sample of quartz-veined Espanola Formation siltstone at L4+80V, 2+OOV from 1988 (sample 3918) Is situated in the area of the fault trace and assayed 351 ppb gold. Perhaps the

-67-

fault has sane economic significance. The fault also shows unit

offset and termination in the Le Scarbo Lake area (Geology Hap,

SV Sheet).

Other northerly fault traces show some unit displacements,

notably a structure displacing diabase and Espanola Formation

limestone in the northeast, Geology Hap, IB Sheet, as well as

Gowganda Formation units to the south (Geology Map, SE Sheet).

A rather well developed northeasterly striking structural

fabric is evident on airphotos and topographic maps. In the

field, a series of apparently brittle faults in this orientation

serve to offset the lo. l and 2 Copper Structures. The Canamlska

Copper Zone apparently occupies a northeasterly structure.

Additionally, some zones of Intense shearing follow this

orientation, especially the 300-foot wide serlcite-chlorite-

carbonate SCS Shear Zone in the northeast of the Jentina

Property, best observed on the Highway 546 road cut. A 1993 grab

sample of shear material assayed 0.068% copper. A narrower shear,

the TSS at approximately L16+OOE, TL10+OOV, contains talc,

sericite +S- actinolite plus chlorite breccia and may displace

the lo. l Copper-Precious Ketal Structure right laterally. A 1988

grab sample of this material which contained quartz-carbonate

veining assayed O.402* zinc. Both the SCS and TSS are indicated

on Geology Map, IV Sheet.

Significantly, these BIB structures trend sub—parallel to

oblique to the regional Flack Lake Fault (System). perhaps

representing conjugate or subsidiary fractures/faults.

-68-

Some mineralization Is known along the trace of the Flack

Lake Fault. In the northwestern part of the property, a

continuous chip sample across 2 feet of quartz vein-chlorite

schist within the Flack Lake Fault Zone assayed 0.392 copper

(1988, sample 3902). Chalcocite, chalcopyrite and malachite were

identified in the vein material.

A few northwesterly structures are indicated in the north-

central part of the property (Geology Hap, W Sheet). The 1988

soil geochemical survey uncovered some anomalous gold, copper and

zinc anomalies over diabase which trend northwesterly, perhaps

indicating some mineralized quartz veins. The anomalies occur in

the southeast portion of claim 1118612.

Topographic considerations suggest some east-west

structures. Two such faults are indicated; along the diabase

through Lost Lake, southern part of claim 1118612, and south of

the diabase In a low—lying flat area across northern claim

1118696. Additionally, quartz stringers occur in Gowganda

Formation siltstone west and southwest of Le Scarbo Lake, close

to a low-lying east-west running creek and swampy area. An east-

west striking shear or fault is Interpreted. Significantly, the

To.l and 2 Copper Structures trend east-west (Section 7.4).

Some folding is Indicated on the Jentina Property. As

previously mentioned, a synformal structure in Espanola Formation

siltstone is indicated at the western end of the diabase sill. An east-west striking antiformal axis is indicated from bedding

measurements through the Bar Biver Formation exposure centered at

-69-

L23+OOE, TL10+OOV. Support for the northeasterly striking Little Vhite River Anticline Is provided by bedding features in Espanola Formation lithologies in the area of L16+OOV-12+OOV, 11+001 and

L12+OOV-L8+OOV, BLO+00. Some weak copper (up to 0.1131) and zinc

Cup to 0.0201) mineralization In quartz velning and breccia

hosted by Espanola Formation limestone was previously considered

to be related to the fold axial trace, however the velning trends

northwesterly.

7.4 Copper and Precious metals-Bearing Structures

Two linear mineralized structural zones, one located north

of the central diabase sill, the other to the south, were delineated during the field program. These copper-rich structures represent a class of polymetallic, probably epithermal to mesothermal quartz—chlorite breccia veins and chloritic shears widely recognized throughout the Huronian Basin. Among the characteristics of these deposits Is pervasive to scattered

albite alteration and the occurrence of unevenly distributed,

high-grade (Cu-Zn-Pb-Ag-Au), massive sulphide "shoots".

Numerous breccia textures, late quartz-carbonate velning and

massive sulphide "horizons" are recognized in the Jentlna showings and are described following. The principle mappable

alteration and structural features on the main claim block are listed in Table 6.

-7O-

Table 6:

miEKALIZED) BKECCIA/YEIY ZOMBS and associated ALTERATION

C ... chlorite alteration zone with some associated shearing and Mineralization

AQ ... alblte-slllca alteration zone

BZ ... quartz-chlorite +X— albite breccia zone with BOMB Fe—carbonate

AA ... albite alteration

QCV .. late quartz—carbonate veinlng, stringers and stockwork

TSS .. talc-sericlte (actinolite?)-chlorite schist/breccia zone

SCS .. sericite—chlorite (+X—carbonate) schist

7.4.1 lo. l Copper—Precious Ketal Structure

This structure is traced more-or-less continuously froot L2+OOV, TL10+OOW to approximately L33+OOE, 16+001*. a distance of 3,500 feet. It is cut off to the west by a northerly fault structure and to the east by a WE-striking fault, however it should be emphasized that the area of Espanola Formation lithologies east have not been well prospected. Some old trenches occur at L40+OOE, 15+OOff in an area of poor exposure. Themineralized structure varies In width from 30 to 150 feet wide and in some areas there is considerable cover and the zone may be wider. The structure is offset by numerous, mainly northeasterly,late faults and both dextral and slnstral diaplacements are^•—*.

. noted. A northeasterly fault cutting the structure in thevicinity of L18+OOE, TL10+OOE apparently displaces the structure

-71-

350 feet left laterally. The talc-chlorite (-actinolite) shear TSS is also terminated by this fault. Some displacement across northwesterly-bearing faults is also evident (Geology Hap, HE Sheet).

The main host is Espanola Formation llaestone/dolomite, however this unit contains narrow (to 3 feet) beds of siltstone. Siltstone and cherty siltstone host is common in the area of L20+OOE to L29+OOE, along the edge of the high ridge of Bar Biver Formation quartzite. At least part of the structure is Indicated to follow an Espanola Formation - Klssissagi Formation (sandstone) contact; L10+OOE - L20+OOB. The structure seems to trend parallel to local bedding, dipping steeply to the north vs the shallower bedding attitudes.

At the east and west ends, the structure is bordered by a chlorite alteration or chloritic shear zone, enveloping the sulphide-bearing breccia vein and alteration zone. The chloritic material is also mineralized with disseminated chalcopyrite and quartz stringers. Considerable malachite staining is common (Plate 16).

The west end of the zone forme a relative topographic knoll with a rather sharp north-south edge. This section was blasted during 1993, forming a clean rock face measuing 60 feet long, designated Trench 1. Figure 24 shows the general geology and chip channel sample sites across the trench (east) face. Chloritic shear material clearly encloses the structure and dips steeply to the south. Some unaltered limestone and siltstone selvadegs or

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T

K •*

C to

e T

B e

-ZL

-

-73-

xenollths of various size and form are common In the quartz- chlorite breccia zone to the north.

The main body of the structure consists of irregular quartz- chlorite breccia with considerable unevenly dlstlbuted albite - silica alteration. This material contains irregular pods up to 2 square feet of semi—massive pyrite and chalcopyrite, roughly 5* of the zone. lumerous scattered disseminations and large (2 inches) blebs of chalcopyrite occur in the quartz-alblte alteration zone, apparently showing preference for north - northeasterly fractures (Plate 12). Some late quartz +X- carbonate veins cross the zone, both parallel to the east-west trend (Plate 10) and as relatively flat-lying eactenslonal features running north-south (Figure 24).

Plates 10-11 and Figure 24 show that bedding features are quite diseernable and some gentle warp-like folding is observed. Some of these folds may have been generated by the numerous southerly dipping to vertical mesoscopic faults. Plate 11 shows a rather broad section of unaltered laminated siltstone beneath pervasive albite-slllca alteration.

Chip channel sample results are shown on Figure 24. Detailed rock sample descriptions are provided in Appendix E. The best samples returned O.6301 Cu over 4.0 ft. and O.4451 Cu over 10.0 ft. A 1993 grab sample assayed 1.261 Cu.

Bo gold values were returned from this sampling program, however 4 grab samples sent for anaylsls to Soyal Oak Kines Inc. returned the following gold assays:

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Samnle Au An •L n't i. onCppb) (oz/T)

12151 855 0.025

12152 480 0.014

12153 410 0.012

12154 995 0.029

llmestone(?); sil w l* bands of qtz, IX bornite

chloritic shear; qtz bands, 1-42 chalcopyrite

albite-sillca alte; 1- chalcopyrite, 12 bornite In late fractures

albite-sillca alte; fg sulphides, coarse chalcopyrite

A 5-foot vertical channel sample of sulphide-bearing quartz chlorite from small Trench la (Ll+OOV, TLlO+OOff) assayed O.305* Cu. The chalcopyrite blebs generally align with a series of northerly fractures (Plate 12).

The zone of mixed quartz—chlorite breccia and albite-sillca alteration persists east to approximately LO+50V. Grab sample 9412 of this material contains 216 late quartz-carbonate ve in Ing and 31 stringers and blebs of chalcopyrite. The sample returned 0.302 Cu.

Trench 2. a narrow and shallow north-south trench located at Ll+OOE, TL10+OOF, cut an Impressive 35-foot wide zone of quartz- chlorlte with some albite breccia and late, more-or-less structure parallel, quartz-carbonate velnlng (Figure 25). Sample 9416, which assayed 1.882 Cu over 5 ft., consists of 20X quartz- carbonate veining and breccia in chlorltlzed limestone. A narrow C4") band or lense of 452 chalcopyrite is contained in the Interval.

A sulphide-bearing, 8"-wide quartz vein containing 22

-75-

^ C*uA4/

•v

o- o-

J6'

Figure 25: Trench 2, east face: geology, sample sites and assay results

-75-

chalcopyrite, 10* malachite and some pyrite, was channeled from a small trench at L2+OOE, TL10+OOV. The vein Is hosted by quartz- chlorlte breccia. A 5-foot sample returned 1.041 Cu.

A 6-foot long east-west trench was blasted at approximately L3+OOE, TL10+OOM In a zone of pervasive albitization, about 1.5 ft. wide. Excellent quartz-chlorite-alblte breccia adjoins the albite zone to the south. The breccia contains numerous angular albite fragments up to 3-5" long.

The Main Showing area at L31+OOE, 16+OON provides the best localization of mineralization along the trace of the Ho. l Copper-Precious Metal Structure. This was the focus of much of the Fort lorman work in 1974 (Section 3.11). The dispositions of the various pits and trenches is diagramed in Figure 26.

Fit l, Pit 2 and a small cut to the east of Pit l were blasted' and sampled in 1993. A grab sample from Pit l assayed 8.10* Cu and 0.76 oz Ag/T; another from Pit 2 returned 4.64* Cu. The best of three, 3.3 foot chip channels returned 5.30* Cu. Previously in 1988. United Reef reported 8.98* Cu and 0.02 oz Au/T over 13 ft. (Section 3.1.14).

Pit l was re-examined and sampled during the 1994 program. Geology and chip channel sample sites are shown in Figure 27. This showing contains considerable chalcopyrite—bearing quartz- stringers and veinlets in both the chloritic shear or alteration envelope CPlate 16J and across the quartz-chlorite breccia zone (Figure 27). Malachite and some azurite and hematite staining is also abundant. Several bands of massive sulphide (pyrite-

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-77-

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-

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-78-

chalcopyrite) measuring up to 8" wide are found from place-to-

place and apparently follow bedding planes or perhaps a

subparallel fracture/fault (Plate 15). The plate also shows

folding of the host cherty limestone (lower right) and siltstone

(upper left).

The degree of schistosity and some faulting is well

illustrated in Plates 13 and 14. Sample sites are also depicted.

Chip channel sample assay results are given in Figure 27. The

best result was from 9422 which crossed some semi-masslve

sulphide horizons containing 201 chalcopyrite, plus 151

chalcopyrite and some bornite, pyrite in late quartz

vein/stringer material. The sample returned 6.78* Cu, 1.90 oz

Ag/T plus some gold over 8 ft. Sample 9424, over 6 ft., assayed

O.80* Cu and 0.03 oz Au/T In a quartz vein-rich quartz-chlorite

breccia zone. Some portions of massive pyrlte-chalcopyrite pods

to 5" were included In the sample.

7.4.2 To. 2 Copper Structure

This more-or-less east-west striking mineralized structure

is poorly exposed over a length of approximately 4,400 ft., from

L48+OOY, 4+OOS to L4+OOV, 4+50S ('94 grid). Continuity over this

distance is assumed as exposed portions of the zone occurs at the

same relative station on 7 of the 12 lines, which to date, are

indicated to cross the structure. The zone was not detected to

the west of L48+OOY, however the orientation of the structure is

on a direct line to the Little White River Lead Mine (Section

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3.1.1) situated 3,000 feet in that direction. The grid east of

L4+OOV was not mapped, hence the structure is open in that

direction. It measures 50 - 300 feet wide, as indicated on

Geology Hap, SE Sheet.

The structure crosses three major rock units, Serpent

Formation feldspathic quartzite in the west. Gowganda Formation

conglomerate and in the east and Espanola Formation siltstone

across most of its length, indicating the feature may be a

previously undetected regional fault/shear zone.

As is observed in the f o. l Structure, several north to WE

trending faults show displacments of up to 100 feet.

The zone consists predominately of chloritized and sheared

siltstone and conglomerate characterized by considerable gossan

and carbonatization. Shear zone orientations are mainly steep to

the south with bedding subparallel and not as steep. Some north

dipping schistositles CS2?) are also noted.

The best section of quartz—chlorite—albite +X— carbonate

breccia occurs In the vicinity of L32+OOY, 2+0OS and Is sited

along the trace of a northeast trending fault at the intersection

with the lo. 2 Copper Structure. Although rock samples from this

exposure returned 80 ppm copper and nil gold and silver, the

alteration and breccia textures are similar to that observed at

the western end of the Jo. l Copper-Precious Metal Structure. Some

brecciation and chloritization in siltstone at L28+OOV, BLO+00

lies along this fault, consequently this northeasterly feature

may warrent furthur investigation.

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Low copper values are returned from grab samples of

sulphide-bearing quartz veinlets hosted by chloritlzed and

sheared Espanola Formation siltstone, for example sample 9433

(O.300ft Cu), 9435 (0.210* Cu) and 9437 CO.086ft Cu). The quartz

veinlets trend subparallel to the trend of the Ho. 2 Copper

Structure, dipping steeply to the south, All of the samples

contain disseminated to blebs of chalcopyrite with some pyrite

and varying amounts of hematite and malachite. Some quartz-

chlcrite breccia is occassional associated, but is not as

pervasive as the lo. l Structure. An exposure of pyritic albite-

slllca altered rock is located Just north of the 0.086ft Cu

outcrop at L12+OOW, 5+10S.

Some Gowganda Formation siltstone at L24+OOV, 6+50S is

carbonatized and contains considerable chlorite, pyrite and

magnetite. The outcrop is either part of the lo. 2 Structure or

has been affected by the adjacent northerly fault trace.

Quartz veining and irregular quartz stockwork with attendant

silicification best describe the ffo. 2 Structure in Serpent

Formation at the west end. Only traces of pyrite occur in vein

material, however some low copper was assayed from three grab

samples; 9430 - quartz stockwork material, 0.012ft Cu, 9431 -

quartz vein within stockwork, 0.043ft Cu and 9432 - quartz vein,

0.017ft Cu. The quartz veins trend oblique to that of the Ho. 2

Structure.

The best exposure of sulphide—rich quartz veining with

associated chloritic shearing occurs in the Southeast Trench at

-SI-

9440O. 175Z Cu/5.O'

9441l. 83-Z Cu/4. O

Of. Tot

V—— M——JL-JLJ

-——— /ST

S f err* f

94421.22* Cu/6.0'

i** f 1

Figure 28: SE trench, west face: geology, saaple sites and assay results

-82-

L3+50V, 4+75S (Figure 28). The main trench measures 100 feet long

and Is up to 9 feet wide to a variable depth of approximately 10 feet. It Is terraced eastwards down the side of a large outcrop

area (Gowganda Formation conglomerate), following the strike of a

sulphide-rich quartz vein system (Geology Hap, SB Sheet, Plates

17 and 18). Two chip channels for a combined 9-foot width were

taken across the zone at the first terrace close to the western,

upper end of the trench (Plate 17). The northern sample, 9441,

cavers the main quartz vein which measures 3 feet wide. It dips

variably to the south to vertically. The vein contains 251 semi-

massive patches of chalcopyrite, pyrite and possibly galena. Some

sheared and quartz-carbonate veined (stringers) host rock

material was Included with the sample which assayed 1.33* over

4.0 ft.

The 5—foot sample to the south, sample 9440, consisted of a

quartz-carbonate stringer zone in chloritic, schistose

conglomerate with some minor chalcopyrite. It ran O.1751 Cu.

A channel across the vein system from the second terrace, 15

feet to the east, assayed 1.221 Cu over 6 ft. (Plate 18).

Scattered trenching and pitting was carried out westwards

along the zone for an additional 150 feet, le the total

continuous length of this mineralized vein zone Is 250 feet. A

grab sample of vuggy quartz—carbonate vein material containing

1571 chalcopyrite assayed 13.001 Cu. The sample is debris from the

most-westerly trench (Geology Map, SE Sheet).

A grab sample from a 1-foot wide chloritic and gossan-

-83-

stained shear contained a l" wide quartz vein mineralized with 22

chalcopyrite and 102 malachite. The sample C9439) assayed O.1352

Cu and le located at L4+OOY, 5+OOS, 25 feet south of the

Southeast Trench area.

7.4.3 Concluding Remarks

Field observations indicate that the two mineralized

structures represent significant fault and shear zones which

likely were generated during reverse faulting along the Flack

Lake Fault system as part of Penokean deformation. The zones run

parallel to the Flack Lake Fault and may be viewed as subsidiary

features.

The mineralization is Indicated to be a poly-phase event

consisting of; 1) shearing accompanied by some brittle fracturing

and brecciation followed by 2) later quartz—carbonate velning.

Sulphide and copper mineralization is found in both cases.

The lo. l Copper-Precious Metal Structure is ascribed

mainly to CI); it is not clear if the breccia textures resulted

from fault-like brittle fracturing, or represent a "blow-out"

feature, perhaps feeding off a larger deep—seated breccia—pipe or

felsic intrusive. The author favours the latter scenario for the

following reasons:

a) The host rock lithology is relatively soft, plastic-like limestone and likely would not produce the very hard quartz- chlorite breccia observed by merely faulting. Some solution was Involved.

b) The presence of albite which is generally associated with Au-Cu-bearing breccia pipes and veins in the region and held to be a metasomatic feature associated with intrusive activity. According to regional studies, albitization is post-Penokean.

-84-

c) aeromagnetic surveying shows a strong circular magnetic low feature centered more-or-less over the Main Showing (Figure 5); a burled breccia pipe?

Alternatively, Intersecting faults may produce breccia.

Some later quartz-carbonate velnlng cuts the Jo. l Structure

and in some places quartz-carbonate breccia is observed

suggesting this material may represent a pre- or syn-velnlng

event at the time of the "blow-out".

The lo. 2 Copper Structure is characterized by quartz-

carbonate velnlng hosted by a chloritic shear zone. As yet, no

significant brecciation is apparently associated, except in the

vicinity of cross-faults. Some quartz stockwork is evident in

Serpent Formation feldspathic quartzite at the western end.

Little albite is associated. This zone is considered to be mainly

a mineralized quartz-carbonate vein system, typical of many area

Fenokeon-type (polymetallic) veins.

Both structures are offset by younger northeasterly and

northwesterly faults. The significance of these structures to

mineralization is not clear, if any, however, the best assays

from the Vo. l Structure occur in the vicinity of cross-faults.

-85-

8. O COICLUSIOKS

The Jentlna Property is situated adjacent and partly overlying the regional Flack Lake Fault, a reverse thrust fault, a prior Archean nornal fault re-activated during the Penokean Orogeny. The fault zone is probably the northern boundary of the Huronian volcano-sedimentary basin with provenance being the Archean hinterland to the north and northwest.

Geological napping on the property indicates that the curvilinear, locally east-west trending Flat Lake Fault System has produced considerable ductile shearing and brittle deformation within the nearby host rocks across the northern Huronian Basin.Several copper-precious metal showings on the Jentina Property are indicated to be associated with east-west striking shear and fault zones, Including the trace of the Flack Lake and Endakai Lake faults.There is no record of detailed structural studies in the region implying many mineralized structures are yet to be discovered.

In particular, two mineralized, approximately east—west structural zones are delineated on the Jentina claims during the mapping program and show brittle to ductile deformation effects:

1) The Ho. l Copper-Precious Metal Structure, located north of the central Nipissing diabase sill, is traced over a length of 3,500 feet. It is poorly explored to the east. Vhere exposed the structure measures 30 to 150 feet wide. The main host rock is Espanola Formation limestone.The best assay results were returned from Pit l at the Main Showing at L31+OOE, 16+OOT, the eastern-most extent of the structure discovered to date. An 8-foot channel sample assayed 6.782 Cu, 1.90 oz Ag/T (1994). Some gold was returned from channel sample 9424: 0.802 Cu and 0.03 oz Au/T. A 1993 grab sample returned 8.102 Cu, 0.76 oz Ag/T.At the east end in Trench l (L2+OOV, TL10+OOF), the best channel sample returned O.63* Cu over 4.0 feet. A grab of albite— silica material returned 0.029 02 Au/T. A sample from Trench 2, 300 feet to the east, assayed 1.882 Cu over 5.0 feet.The structure is characterized by quartz-chlorite breccia and albite-slllca alteration, features typical of many area Au-Cu veins and breccia pipes. The main sulphides include pyrite and chalcopyrite which occurs in semi—massive bands more-or-less parallel to steeply dipping cleavage Cor bedding?) and as disseminated blebs or pods, frequently aligned with cross-cutting fractures in alteration zones and as disseminations in quartz str ingers/veins.

-86-

2) The lo. 2 Copper Structure, located south of the diabase sill. Is exposed east-west for 4,400 feet. Jo napping/prospecting was carried out along strike to the east. To the west, the structure is on a line with the Vhite River Lead Mine, 3,000 feet away. Grab sampling of quartz vein debris at the mine by the Ontario Department of Mines in 1969 yielded 3.46 oz Ag/T, 0.10 oz Au/T, 1.561 Cu plus some Pb, Zn, Co, Bi.

The best assay from the lo. 2 Structure was returned from the Southeast Trench: 1.83* Cu over 4.0 feet. A grab sample of semi-massive chalcopyrite from a pit 150 feet to the west assayed 13.001 Cu.

The structure crosses a variety of host rocks, characterized by sulphide-rich quartz-carbonate veins in chloritic shears in Espanola Formation siltstone and Gowganda Formation conglomerate and as quartz stringers, stockwork in Serpent Formation feldspathic quartzite.

The If a. 2 Structure is concluded to represent the class of polymetallic) quartz vein-hosted deposits found within the Huronian Basin, emplaced during the Penokean Orogeny, and may represent a previously un-recognized fault zone parallel to the Flack Lake Fault Zone, or perhaps part of this system.

Age dating Information and field relationships indicate that all mineralization post-dates Vlpissing diabase intrusion.

Other areas of known significant copper-precious metal mineralization worthy of exploration on the Jentina claims include:

a) Canamiska Zone; a 9,600-foot long EM conductor and copper in soils anomalous geochemical zone occupying an EVE-trending structure. The best drill Intersection f. 1965) was 1.44ft Cu over19.5 feet (hole 65-7). Apparently no drilling was carried outover the northeastern, part of the zone where soil values of up to 6,000 ppm are reported.

b) Flack Lake Fault Zone; grab samples from an east-west striking quartz-carbonate zone assayed up to 15.63* Cu, 0.24* Zn, 0.36 oz Ag/T and 0.02 oz Au/T (1978).

A 2-foot chip channel along the trace of the Flack Lake Fault at the northwestern corner of Jentina Main Block assayed O.390* Cu (1988).

A 4 to 6-foot wide northerly trending shear extends from the Flack Lake Fault on the Triangle Lake Claims. Grab sample assays of up to 7.45* Cu and 0.28 oz Ag/T are reported from copper sulphide-rich quartz veinlets (1971). Some disseminated mineralization in the host rock ran 1.6* Cu and 0.15 oz Ag/T.

A copper in lake sediment anomaly from Triangle Lake gave 980 ppm. The trace of the Endakai Lake Fault crosses the lake.

-87-

c) Bruce-Presto Zone; a 500-foot long shear zone in diabase on a patent claim adjoining the northeastern corner of the Jentina Property, Main Block, reported copper-cobalt values of 2- 3* Cu and trace-2% Co (1950's). The zone is Indicated to dip south onto the Jentina claims. 1964 drilling on the Jentina ground and south of the showing returned assays of up to l. 96X Cu over 11.5 feet In host Espanola Formation siltstone.

d) Various soil geochemical areas; two broad areas of anomalous soil geochemical metal values are recognized (1988): an area of elevated Cu-Ag-Au over the Hississagi Formation sandstone north of the Little White River and an area of Cu-Zn underlain by Espanola Formation lithologies north of the central nipissing diabase sill. Although generally considered to be due to the numerous metalliferous quartz-carbonate veinlets/velns In these areas, a possible SEDEX derivation should not be dismissed out of hand. Some sedimentary copper mineralization is reported at the Lorrain-Gordon Lake Formation Interface 20 miles east of the property.

Structural-mineralogic and aeromagnetic features at the Ho. l Copper-Precious Metal Structure suggest the most likely target for economic mineralization on the Jentina ground is polymetallic (Cu-Ag-Au) mineralized breccia zones or pipes similar to the Proterozoic Olympic Dam deposit in Australia and the Wernecke Mountains deposits of the Yukon.

Other possible primary exploration targets are listed following.

- Sufficient grade and tannage may exist in quartz-veinhosted copper (-polymetallic) vein-style mineralization, forexample the Ho.2 Copper Structure and the Canamlska Zone.

-"Greenstone" (Huronian volcanics?) at a vertical depth of approximately 250 feet was intersected in Canamlska drill holes. Atlantic Bichfield drilling in 1967 intersected "Archean" volcanics at a depth of approximately 4,000 feet Just north of the Ho. 2 Copper Structure. Archean volcanics are indicated to outcrop Just north of the Jentina Property.

Although no significant VMS-style of mineralization has been discovered in the region, the presence of both Archean and Proterozoic volcanics in the vicinity of Jentina suggest volcanogenic massive sulphide mineralization Is a target on the property.

- The Flack Lake Fault Zone, demonstrated to be a regional unconformity between Huronian supracrustals to the south and Archean rocks to the north, has imparted various ductile to brittle deformation effects on area host lithologies. Regional unconformities or deformation zones are common sites for the localization of Archean-style auriferous quartz vein deposits.

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The Flack Lake Fault System nay provide gold targets.

9. O

Two approaches to furthur explore the property should be considered; 1) exploration follow-up of the two main known zones of mineralization which would entail mechanical stripping and diamond drilling and 2) detailed evaluation of the entire Jentlna claim area, including the outlying areas not yet investigated. The second approach would consist of detailed griding of all or parts of the property, le 100-foot spaced lines with 50-foot stations, stressing detailed magnetometer surveying and structural mapping, lithogeochemical sampling. Both structural details and litogeochemistry are lacking for this part of the Huronian Basin. The role of EH or IP surveying in this district is not well established and some test surveying may be advantageous.

The advantages to the second approach is two-fold:a) to provide a structural synthesis of the property possibly determining the controls of the known mineralization, as well as aiding in the discovery of other zones. The study will investigate structure intersections, various magnetite features, confirm the cause of the aeromagnetic circular feature, etc. The relationship of the property structures to the Flack Lake Fault System may be determined.

b) establish a lithogeochemical database from which alteration features may be determined and signatures of buried mineral deposits, such as polymetallic breccia pipes and VMS deposits, may be outlined.

The second approach will provide the most information to allow selection of the optimum diamond drill targets. The following exploration proposal and budget is forwarded:

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pfoase la; llnecutting. geophysics. structural lithogeochemical sampling

Llnecutting200 miles (320 Km) 9 SSOO/mlle ... 560,000

GeophysicsMag/VLF-EX 380 Km 9 4200/Km . . . . . . . 76,000Test IP/EH 20 Km 9 Sl.SOO/Km . .... 30.000

106,000 106,000

Structural Happing, Lithogeochemical Sampling

Senior Geologist,Project Supervisor 90 days 9 5275/day ... 24,750 Geologists (2) 180 mandays 9 S225?day ... 40.500

65,250 65,250 GST on professional fees 4,567

Support CostsFood, accomodation

270 mandays 9 3125/day ... 33,750 Truck, ATV rentalsS5,000/month for 3 months ... 15,000 Miscellaneous supplies 2.OOP

50,750 50,750

AnalyticalAssay, 200 samples 6 SSO/sanple . . . .... 6,000Whole Rock, 200 samples 9 940/sample . . . . . . . 8.000

12,000 12,000

Reporting, drafting ...... 20.OOP

318,567 say S319,000

plus 10t4 Administration, Contingency 31.900

Total phase la 350,900say 5350,000

phase Ib; mechanical stripping and sampling

Backhoe w Operator30 days 0 5350/day . . . . . . . . . . 410,500

Sampler, Geological Technician30 days 9 8175/day . . . . . . . . . 5,250

Geologist 15 days 9 3225/day . . . . . . . . . 3.3758,625 8.625

GST on professional fees 604

-90- Support Costs

Food, AcconodatIon45 mandays fi 5125/day . . . . . . 5,625

Truck, ATV rental . . . . . . . . 3,000

Miscellaneous Supplies . . . . . . . . 1.OOP9,625 9,625

Analytical200 assays fi 530/sample . . . . . . . . 6.000

35,354 say 535,500

plus I QTt Administration, Contingency 3.550

Total phase Ib 39,050say 539,000

Total phase l 5389,000

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phase 2 i Drilling

Road Building

Drilling 20,000 feet fi 520/foot

Geologist 60 days fi S250XdayGST on professional fees

Support CostsFood , Accomodat i on

60 days fi 5125/day Truck, ATV rental

S2,OOOXmonth Miscellaneous Supplies

plus 1071 Administration, Contingency

Total phase 2

Total phase l and 2

say

520,000

400,000

15,0001,050

7,500

4,0001.000

447,5505448,000

44.800

492,8005492,000

•881.000

Respectfully submitted Date: September 15, 1994

F.O. Willoughby, B.Se.(Hons.)

KHFKKEBCHS

Anthony, E.G. and Willoughby, 1988: Report on geological and soil geochemical surveying of the Albanel copper-gold property: Unpubl report for United Reef Petroleums Limited, Oct., 1988, 54 pgs.

Atkinson, V. V. , Kacmarowskl, J. H. and Erlckson, A. J., 1982: Geology of a skarn-breccia orebody at the Victoria Mine, Elko County, Sevada; Econ. Geol. v. 77, no. 4 p 899-918.

Bennett, G., Dressler, B.O. and Robertson, J.A., 1991: TheHuronian Supergroup and associated Intrusive rocks, pp 549- 592 In Geology of Ontario, Ont. Geol. Surv., Spec. Vol. 34, part l, 711 pgs.

Chandler, F. Y., 1984: Sedimentary setting of an Early Proterozoic copper occurrence in the Cobalt Group, Ontario: a preliminary assessment; p 185-192. in Current Research, Part A, Geol. Surv. Canada, paper 84-1A.

Ennls, G.F., 1955: Diamond drill logs for Plcton Uranium Hlnes Limited; Assessment file Albanel 0012, Resident Geologist's Office, Sault Ste. Marie.

Fyon, J.A., Bennett, G., Jackson, S.L., Garland, X.I. and Easton, R. H. , 1992: Metallogeny of the Proterozoic eon, northern Great Lakes region, Ontario, pp 1177-1217 In Geology of Ontario, Ont. Geol. Surv., Spec. Vol. 4, pqrt 2, 1525 pgs.

Gauthier, V . , Rocheleau, K., Kelly, D. and Gagnon, T., 1990: Controls on the distribution of gold mineralization within the Cadillac Tectonic Zone, Rouyn-Beauchastel Segment, Abitibi, Quebec; In The Northwestern Quebec Polymetallic Belt: A SuT|nroi r'y of 60 Years of Mining Exploration; CIMH Spec. Vol. 43, K. Rive, P.Verpaelst and others, editors, p 185-198.

Gasch, J.V. and Vogel, T.A., 1959: Unpubl geology map, Univ. of Vlsconsin; Assessment files, Resident Geologist's Office, Sault Ste. Marie Mining Division.

Gowganda Silver Mines Limited, 1972: Geological plan, Groups a ft B, Twp 163; from ODM Map P.560.

GSC, 1987, Regional lake sediment and water geochemical reconnaissance data, Ontario, VTS 41J, Geol. Surv. Canada, Open File 1356.

Hanna Mining Company, 1969: Diamond drill log, hole 16; Assessment file Albanel 0017, Resident Geologist's Office, Sault Ste. Marie.

Hltzman, X. V., Oreskes, F. and Einaudi, H.T., 1992: Geological characteristics and tectonic setting of Proterozoic iron- oxide ^u-U-Au-REE) deposits; Precam. Res. , v. 58, p 241- 287.

Hubert, C., Trudel, P. and Gellnas, L., 1984: Archean wrench fault tectonics and structural evolution of the Blake River Group, Abitibi Belt, Quebec; Can Jour Earth Sci., vol. 21 no. 9 p 1024-1032.

Innes, D.G. and Colvine, A.C., 1990: Metallogenetic development of the eastern part of the Southern Province of Ontario; in Summary of Field, Ont. Gecl. Surv. SP 90, p 184-189.

Laznlcka, P., 1988: Breccias and Coarse Fragmentltes; petrology, environments, associations, ores; developments in economic geology 25; Elsevier, Tew York, 832 pgs.

McKecknie, D.C., 1964: Report on the property of Bruce-Presto Mines Limited in Townships 163 and 169, Sault Ste. Marie Mining Division, Ontario, 3 pgs with drill logs; Assessment file Albanel 0028, Resident Geologist's Office, Sault Ste. Marie.

Moore, E.S., 1930: Ore deposits near the Forth Shore of Lake Huron; Ont. Dept. Mines Ann. Rep, v.38, pt. 7, p 1-51.

Herman, D.I. and Sawkins, F.J., 1985: The Tribag breccia pipes: Precambrian Cu-Mo deposits. Batchawana Bay, Ontario; Econ. Geol. vol. 80, no. 6 p 1593-1621.

OGS, 1993, Single master aeromagnetic data; Ont. Geol. Survey, ERLIS Data Set 1.

Pearson, V.V., 1978: Copper metallogeny, Lake Huron area, Ontario; Geol. Surv. Canada, Paper 78-1A, p 263-268.

Pearson, V.V., 1979: Copper metallogeny, north shore region of Lake Huron, Ontario; Geol. Surv. Canada, Paper 79-1A, p 289- 304.

Richards, J.P. and Spooner, E.T.C., 1989: Evidence for Cu-(Ag) mineralization by magmatic-meteorlc fluid mixing in Keweenawan fissure veins, Mamainse Point, Ontario; Bean. Geol., v. 84, p 360-385.

Robertson, J.A., 1969:ant. Dept. Mines geology map, Map 2347, Nicholas and Raimbault townships, scale 1:31,680.

Robertson, J.A., 1970: Geology of the Soragge area; Ont. Dept. Mines, GR 76, 109 pgs.

Roscoe, S.M. and Card, K.D., 1992: Early Proterozoic tectonics and metallogeny of the Lake Huron region of the Canadian Shield; Precam. Res., v.58, p 99-119.

Rupert, R.J., 1974: Diamond drill logs for Fort Forman Explorations Inc.; Assessment file Albanel 0015, Resident Geologist's Office, Sault Ste. Marie.

Schandl, E., 1992: Few light on Sudbury-type rocks; Forthern Klner, August 23, 1992, p 5.

Scheerer, P., 1956: Unpubl geology map, Univ. of Wisconsin; Assessment files, Resident Geologist's Office, Sault Ste. Marie Mining Division.

Shklanka, R., 1969: Copper, nickel, lead and zinc deposits of Ontario; Ont. Dept. Mines, MRC 12, 394 pgs.

Siemiatkowska, K. M., 1978: Geology of the Endikai Lake area, District of Algoma; Cnt. Geol. Surv., Report 178, 79 pgs. Accompanied by Map 2399, scale 1:31,680.

Sullivan, D. W., 1967: Diamond drill report for Trlller Explorations Ltd., 9 pgs; Assessment file Albanel 0024, Resident Geologist's Office, Sault Ste. Marie.

Thomson, Jas.E., Ferguson, S.A., Johnstone, V.G.Q., Pye, G.E., Savage, V. S. and Thomson, R., 1957: Copper, nickel, lead and zinc deposits of Ontario; Ont. Dept. Mines, MRC 2, 126 pgs.

Yalford, P.C. and Franklin, J.M., 1982: The Anderson Lake Mine, Snow Lake, Manitoba; p 481-523 in Precambrian Sulphides, H. S. Memorial Volume, edited by R.V. Hutchinson, C.D. Spence and J.X. Franklin; Geol. Ass. Canada, Spec. Paper 25, 791PSS -

Vharton, R.E., 1968: Diamond drill logs for Atlantic Richfield Company; Assessment file Albanel 0013, Resident Geologist's Office, Sault Ste. Marie.

Vllllajns, R. H., 1965-1966: Drill sections at l" ~ 20' and l" = 50' for Canamiska Copper Xlnes Limited; Assessment file Albanel 0031, Resident Geologist's Office, Sault Ste. Marie.

Willoughby, F.O., 1993: Structural controls for gold mineralization at the Granada Gold Mine and Granada Extension properties: delineation of a significant, 8 Km long auriferous shear zone system, the Granada Tectonic Zone; unpub draft report for KVG Resources Inc., 21 pgs.

Zlmmerman, J.R., 1971, 1972: Geololgical report on the Hamilton claim group for Stanford Mines Limited with drill logs; Assessment file Albanel 0020, Resident Geologist's Office, Sault Ste. Marie.

CERTIFICATE OP QU1

I, Veil O. Willoughby, residing at 651 Cosburn Avenue, Toronto, Ontario, do certify that:

1) I an a geologist, a graduate of Carleton University, Ottawa, Ontario, with a B.Se. (Hons.) degree in 1974 and that I have been practising my profession since graduation.

2) I am President of 3TR4J Resource Associates Limited, a consulting firm Incorporated under the Business Corporation Act, 1982, in the Province of Ontario, since August, 1989 and which is authorized by the Association of Professional Engineers of Ontario to engage in the business of providing services that are within the practice of professional engineering under the Professional Engineers Act, 1984.

3) I have a personal 1/5 Interest in the Jentina Hine Property.

4) The statements contained in this report and conclusions and recommendations are based on my observations while so engaged in conducting and supervising field operations during the period June 22 to July 24, 1993 and June 18 to July 18, 1994.

Toronto, Ontario SI *^ *T/Pjtr

Dated: September 15, 1994 Veil O. WilloughbyB. Se. (Hons.)

PLATES

Plate 1:

View south of Iipissing diabase ridge at approximately L64tOOV, 17+OOS ('94 grid)

Plate 2:

Exposed ridge of Gowganda Formation arkosic sandstone with soi granite pebblee; at L24+OOV, 3+OOS <'94 grid)

Plate 3:

View to northwest of Endaka i Lake; fro* the position of Plate 2

Plate 4:

View north-northwest of Archean grani te a long the trace of the Flack Lake Fault, north of the Little Vhlte Fiver; fro* the position of Plate 2

Plate 5:

Ripple aarks and some sluap folding In Bar River Formation quartzite at L25+OOE, 7+50S C'93 grid)

Plate 6:

View west of the Bailey bridge across the from the position of Plate 5

Little Vhite River;

Plate 7:

Ridge of MisslssagI Formation sandstone north of the Little Vhlte River; view north from the position of Plate b

Plate 8:

Graded bedding in Gowganda Formation arkosic sandstone/quartzlte at approximately L12+OOW, 2+75S ('94 grid); stratlgrahlc tops are indicated to be overturned to the north

Plate 9:

SI uiBp f ea t ures l o along the property ('94 grid)

Gowganda ForB access road at

it Ion heterolIthlc conglomerate approximately L36+OOV, TL12+001

Plate 10:

The author standing at the east face, Trench l, of Mineralized quartz-chlorite-albite breccia and quartz-carbonate vein zone In host Espanola Formation limestone and siltstone. Channel samples sites 9402 to the left (0.285X Cu over 6.0 ft.) and 9403 to the right (O.3351 Cu over 5.0 ft.)

Plate 11:

Chris Marehi ldon Measuring strike and dip of siltstone strata (bottom) at the east face. Trench 1. The siltstone is overlain by sulphide-rich quartz-chlorite t/- albite breccia and altered limestone/silt&tone. Channel sample site 9405 (0.093Z Cu over 6.0 ft.) is displayed

Plate 12:

Typical quartz-chlorlte breccia in Trench la at approximately L1+50V, TL10+OOM ('93 grid); Malachite-staining with chalcopyrite blebs show preference for cross-cutting fracture planes

Plate 13:

Chris standing at the east end, south face of Pit l, the Hain Showing; channel sample sites 9423 (1.351 Cu over 9.0 ft.) to the left and 9422 (6.78* Cu, l.9O oz Ag/T and 195 ppb Au over 8.0 ft. y to the right

Plate 14

At the west end, south face, Pit l with channel sample sites 9424 {0.80X Cu and 1,050 ppb Au over 6.0 ft.) to the left, sample site 9425 Cl.OO* Cu over 9.0 ft.) to the right

Plate 15:

Close-up of saaple site 9422 showing aassive sulphide (pyrite- chalcopyrlte-bornite) horizon at lower right and folded Espanola FormatIon llMeetone/siItstone at upper right

Plate 16:

Chloritic shear zone at saaple site 9423 showing •alachlte- stalning and chalcopyrite-bearing shear parallel and oblique quartz veInlets

Plate 17:

View of the west face of the Southeast Trench, 1st terrace, at approximately L3+50V, 4+50S ('94 grid). Chip channel sample site 9441 (1.831 Cu over 4.0 ft.) across the Bain sulphide-bearing quartz vein; chloritic shear zone on either side and with sone quartz-chlorlte breccia

Plate 18:

View of the west face of the Southeast trench, 2nd terrace, 15 ft. east of the location of Plate 17. Chip channel sample site 9442 returned 1.221 Cu over 6.0 ft.

APPEIDICBS

APPEMDII A: Summary Dlaaond Drill Logs

-Al-

A.l Picton Uranium lines Limited, 1955-1968

Hole Jo.___Location______Bearing_______Dip

55-1 ci 25862 350 deg - 45 deg

O - 7.0' overburden7.0 - 20.3' pebble quartzite, Xlssissagl

20.3 - 22.0' quartz vein22.0 - 63.0' pebble quartzite, Mississagi; strongly fractured63.0 - 77.5' quartz pebble conglonerate77.5 - 109.0' quartzite, Mississagi109.0 - 110.5* argillite w quartz110.5 - 140.4' diabase (nipissing)140.4 - 155.0' arkose-quartzite, quartz pebble conglomerate,

Mississagi155.0 - 169.0' diabase (Fiplssing)169.0 - 222.0' arkosic quartzite, quartz pebble conglomerate 222.0 - 308.0' banded cherty sediments, So = 25 deg TGA

EOH (Espanola?-!.O.V.)

Hole Jo.___Location______Bearing_______Dip

55-2 ci 25865 170 deg - 27 deg

O - 55.0' pebble quartzite, Mississagi 55.0 - 106.0' quartzite, Kississagl 106.0 - 140.5' quartz pebble conglomerate 140.0 - 221.0' quartzite w some siltstone, conglomerate EOH

Hole ITo.___Location______Bearing_______Dip

55-3 ci 25867 360 deg -30 deg

O - 6.5' pebble conglomerate 6.5 - 247.0* pebble quartzite, quartz pebble conglomerate;

arkosic in places. 247.0 - 248.6' siltstone248.6 - 278.5* quartzite, hematitlc, Mississagi 278.5 - 298.0* quartzite, argillite, Miselssagi 298.0 - 310.0' quartz pebble conglomerate

BOH

Hole Jo.___Location______Bearing_______Dip

55-4 ci 26275 90 deg

O - 95.0* quartzite w siltstone beds95.0 - 276.0' quartzite, hematitic

276.0 - 289.5' gritty sediment, hematltlzed289.5 - 324.4* quartzite, hematitic

-A2-

324.4 - 334.0' siltstone, hematltized334.0 - 368.0* banded quartzite, henatitlc; So ^ 80 deg TGA368.0 - 412.4' greywacke w 30* hematite412.4 - 472.5' quartzite, henatitlc472.5 - 524.0' siltstone, argillite, hematltlc524.0 - 569.5* henatitlc quartzite w siltstone beds at 80 deg

TGA569.5 - 618.0* diabase, henatitlzed Nipissing?)618.0 - 681.5* quartzite, Xississagi681.5 - 708.0* argillite w So " 75 deg TGA708.0 - 755.0* quartzite, white, porcelain texture755.0 - 765.0* dolomitic limestone (Espanola)

BOH

A. 2 Canaaieka Copper lines Ltd., 1965

Hole Jo.___Location______Bearing_______Dip

65-1 L32+OOE, 15+10H Grid J -45 deg

Lithology Klnerallzatlon

O - 5.0* overburden5.O - 106.0* quartzitic arkose 5. O — 40.0' sulphides106.0 - 147.5* conglomerate 75.0 - 80.0* "147.5 - 161.5* quartzite

161.5 - 192.0* quartzitic arkose 106.0 - 199.0*

C 110.0 - 175.0* - O.106* Cu over 65.0* 9 150.0 - 157.5* - 0.260X Cu over 7.5f

192.0 - 226.0* quartzite226.0 - 250.0' conglomerate 220.O - 240.0' sulphides EOH

9 220.0 - 240.0' - 0.04* Cu over 20.0*

Hole ffo.___Location______Bearing_______Dip

65-2 L32+OOE, 13+85V Grid V - 45 deg

Lithology Kineralization

O - 10.0* overburden10.0 - 19.0* quartzite19.0 - 26.0* arkose26.0 - 92.5* quartzite92.5 - 140.7* arkose 10.0 - 126.0* - sulphides80.0 - 100.8* - 0.04* Cu over 20.8*

140.7 - 243.5* greenstone 243.5 - 263.7' arkose

-A3-

268.7 - 339.5* greenstone 275.0 - 339.5' - sulphides 277.0 - 323.5' - brecciated

6 275.0 - 285.0' - 0.05* Cu over 10.0*6 295.0 - 310.0' - 0.03* Cu over 15.0*e 315.0 - 325.0' - 0.03* Cu over 10.0'

339.5 - 363.0' 363.0 - 454.0*

EOH

Hole Jo.

arkose greenstone

Location Bearing Dip

65-3 L36+OOE, 20+OOF Grid S

Lithology

- 45 deg

Hineralization

O - 25.0'25.0 - 50.0'50.0 - 75.0'75.0 - 91.0*91.0 - 141.5'

overburden arkosearkose, tuff greenstone arkose/tuff 25.0 - 150.0* - sulphides

30.0 - 40.0' - 0.06* Cu over 10.0'48.0 - 58.0* - 0.03* Cu over 10.0*70.0 - 75.0' - 0.03* Cu over 5.0*85.0 - 95.0* - 0.06* Cu over 10.0*

141.5 - 317.0' 317.0 - 323.5* 323.5 - 338.0* 338.0 - 350.0'

EOH

greenstone arkose/tuff greenstone arkose/tuff 338.O - 350.O' - sulphides

6 335.0 - 350.0* - 0.11* Co over 15. O*

Hole Jo. Location Bearing Dip

65-4 L20+OOE, 6+OOff Grid H

Lithology

- 45 deg

MineralIzationO - 19.0*

19.0 - 84.0*overburden arkose 19.O - 84.O* - sulphides

C 30.0 - 40.0* - 0.07* Cu over 10*

84.0 - 111.7* conglomerate111.7 - 181.5* arkose161.5 - 201.0* greenstone201.0 - 218.0* arkose/tuff218.0 - 257.9' quartzitic arkose

84.0 - 350.0' - scattered narrow sulphide sections

-A4-

257.9 - 350.0' greenstone BOH

Hole So.-——-Location_____Bearing————^Dip

65-6 L32+25E, 16+25F Grid S -45 degLithology Mineralization

O - 4.0' overburden4.0 - 20.0' quartzite

20.0 - 46.0' arkose 4.O - 46.0' - sulphides9 5.O - 3O.O* - O.532* Cu over 25.0* C 20.0 - 25.0* - 2. GOZ Cu over 5. O*

46.0 - 67.0' quartzite, arkose67.0 - 90.0* quartzite 46.0 - 90.0' - sulphides EOH

9 6O.O - 75.O* - 0.171 Cn over 15.0*

Hole Jo.___Location______Bearing_______Dip 65-7 L32+25E, 16+255 Grid S -30 deg

Lithology MineralizationO - 4.0' overburden

4.0 - 17.5* quartzite17.5 - 40.0' arkose 4.O - 40.0' - sulphides

6 17.5 - 25.0* - 1.71* Cu over 7.5* 6 25.O - SO.O* - 1.21* Cn over 12.5*

or * 17.5 - 3O.O* - 1.44* Cn over 19.5*

40.0 - 69.0' quartzite, arkose69.0 - 95.0* quartzite 40.0 - 95.0* - sulphides EOH

9 90.0 - 95.0* - 0.38* Co over 5.0*

Hole lo.____Location______Bearing_______Dip

65-8 L31+75B, 16+305 Grid S -45 deg

Lithology MineralizationO - 3.0' overburden

3.0 - 24.0' quartzite24.0 - 47.0' arkose

-A5-

47.0 - 90.0* BOH

Hole Jo.

quartzite 24.0 - 90.0' - sulphides

Location______Bearing_______Dip

65-9

0-3.0* 3.0 - 19.0* 19.0 - 59.0*

L31+75B, 16+30H

Lithology

overburdenquartzitearkose

Grid S -30 deg

Kinerallzatlon

3.0-59.0* - sulphides

9 27.5 - 4O.O* - 0.421 Cu over 12.5' * 32.5 - 35.0* - 1.301 Cu over 2.5*

59.0 - 81.0* BOH

Hole Ho.

quartzite 59.0 - 81.0 - sulphides

Location______Bearing_______Pip

65-10

0-3.0* 3.0 - 32.0*

32.0 - 52.0*

L31+25E, 16+30F

Lithology

overburdenquartzitearkose

Grid S - 45 deg

Ml neralisat ion

52.0 - 90.0* EOE

Hole Jo.

10.0 - 52.0* - sulphides

42.5 - 45.0* - 0.321 Cu over 2.5*

52.0 - 90.0* - sulphidesquartzite

Location Bearing Pip

65-11

O - 15.0*15.0 - 36.0*36.0 - 70.0*

L32+75B, 16+601

Lithology

overburdenquartzitearkose

Grid S -45 deg

Mineralization

15.0 - 57.0*- sulphides

42.5 - 50.0* - 1.821 Cu over 7.5* 45.0 - 47.5* - 4.601 Cu over 2.5'*

70.0 - 97.O* BOH

quartzite 60.0 - 97.0* - sulphides

fi 62.5 - 65.0* - 0.63Z Cu over 2.5*

-A6-

* Assessment file shows an averaged grade of 2.51* Cu over 10.0', however two assay Intervals as stated above are shown on the drill section. The 2.51* figure (Incorrect) is shown on Map A.

Hole Jo.___Location______Bearing_______Dio

65-12 L32+25E, 17+OOff Grid S - 45 deg

Lithology Mineralization

O — 7.0* overburden7.0 - 22.0* quartzite22.0 - 46.0' arkose 7.0 - 46.0' - sulphides

® 7.0 - 30.0* - 0.06* Cu over 23.0'

46.0 - 75.0* quartzite75.0 - 93.0* arkose93.0 - 105.0* quartzite 80.0 - 105.0' - sulphides

fi 95.0 - 10O.O' - 0.51* Cu over 5.0*

105.0 - 128.0' quartzlte/arkose128.0 - 160.0* quartzite 105.0 - 150.0' - sulphides

Q 95.0 - 125.0* - 0.17* Cu over 3O.O'C 125.0 - 150.0* - 0.07* Cu over 25.0*

160.0 - 260.0* greenstone EOH

Hole Ho.___Location______Bearing_______Dip

65-13 L33+25E, 16+50V Grid S -45 deg

Lithology Mineralization

O - 10.0* overburden10.0 - 27.0* quartzite27.0 - 75.0' arkose 42.0 - 52.5' - sulphides

e 42.0 - 52.5* - 0.23* Cu over 10.5* C 50.0 - 52.5* - 0.58* Cu over 2.5*

75.0 - 105.0* - quartzite 60.0 - 80.0* - sulphides 105.0 - 125.0' - quartzite/arkose

EOH

Hole If o. Location

-A7-

Bearlng Dip

65-14 L24+OOE, 8+OOff Grid H

Lithology

O - 10.0' 10.0 - 80.0*

- 45 deg

Klnerallzation

overburden quartzitic arkose

80. 120.

163.180.204.

235

0 - 120.0' greenstone0 - 163.6' conglomerate 153.5

9 153.5 - 163.5' - 0.071 Cu over

5 - 180.0' quartzitic arkose0 - 204.0' conglomerate0 - 235.0' quartzitic arkose 200.0

9 200.0 - 225.0' - O. 08* Cu over

0 - 267.0' conglomerate 235.0

9 235.0 - 260.0' - 0.06* Cu over 9 235. O - 242. O* - 0.42* Cu over

- 163.5* - sulphides

10.0'

- 235.0'

25.0'

- 267.0'

25.0* 5.0'

- sulphides

- sulphides

267. 0 - 300.0' EOH

greenstone 270.0 - 280.0' - sulphides

9 270.0 - 280.0* - 0.06* Cu over 10.0'

Hole Bo.___Location______Bearing_______Pip

65-15 L16+OOV, 18+OOV Grid K

Lithology

O15.085.092.0

355.9

15.0'85.0'92.0*355.9'400.0*EOH

overburden quartzitic arkose conglonerate quartzitic arkose greenstone

- 45 deg

Kinerallzation

numerous scattered narrow sulphide sections

Jo.. Location

65-16 L16+OOV, 21+OOH

Lithology

O - 21.0' overburden

- 55 deg

Kineralizat ion

-A8-

21.0 - 56.0' quartzitic arkose56.0 - 59.0' greenstone59.0 - 80.0' quartzitic arkose80.0 - 105.0' greenstone 25.0 - 90.0' - sulphides,105.0 - 131.0' quartzitic arkose low Cu assays131.0 - 142.4' greenstone142.4 - 173.7 quartzitic arkose 126.0 - 136.6* - sulphides

6 126.0 - 136.6' - 0.07* Cu over 10.6'

173.7 - 177.4* greenstone177.4 - 197.4' quartzitic arkose197.4 - 206.5' greenstone 195.9 - 206.5' - sulphides

9 195.9 - 206.5' - 0.05* Cu over 10.6'

206.5 - 233.0' quartzitic arkose 233.0 - 260.0* arkose/tuff 260.0 - 304.0' greenstone

EOH

Hole Ho.___Location______Bearing_______Dip

65-17 L24+OOV, 10+25F Grid I -60 deg

Lithology Kinerallzatlon

O - 107.0* overburden 107.0 - 175.0' quartzitic arkose 107.0 - 125.0';

165.0 - 175.0* - sulphides

9 107.0 - 125.0* - 0.03* Cu over 18.0* 9 165.0 - 175.0' - 0.05* Cu over 10.0'

175.0 - 191.5' arkose/greenstone191.5 - 246.5' quartzitic arkose 235.0 - 246.5* - sulphides

9 235.0 - 246.5* - 0.05* Cu over 11.5*

246.5 — 260.0* arkose/greenstone260.0 - 350.0' quartzitic arkose 270.O - 350.0* - sulphides

EOH

9 310.0 - 330.0' - 0.05* Cu over 20.0*

Hole Jo.___Location______Bearing_______Dip

65-18 L24+OOV, 15+50V Grid H -60 deg

Lithology Klneralization

O - 60.0* overburden

-A9-

60.0 - 214.3* quartzitic arkose 60.0 - 120.0';160.0 - 214.3* - sulphides

9 160.0 - 180.0* - 0.05* Cu over 20.0* 9 180.0 - 200.0* - 0.07* Cu over 20.0*

214.3 - 228.8* greenstone228.8 - 287.5* quartzitic arkose 250.0 - 287.5' - sulphides

9 25O.O - 270.0* - 0.10* Cn over 20.0*

287.5 - 309.0* greenstone 287.5 - 309.0* - sulphides

9 287.5 - 309.0* - 0.05* Cu over 21.5'

309.0 - 435.6* arkose/greenstone 435.6 - 441.0' quartzitic arkose441.0 - 470.0* greenstone 435.6 - 450.0' - sulphides 470.0 - 500.0* quartzitic arkose 470.0 - 500.0' - sulphides

SOB

9 480.0 - 482.5* - 0.17* Cu over 2.5*

Hole Jo.___Location______Bearing_______Dip

65-19 L40+OOV, 25+505 Grid V -45 deg

Lithology Hineralizatlon

O - 12.0' overburden12.0 - 167.5* quartzitic arkose

167.5 - 205.5* greenstone205.5 - 230.0* quartzitic arkose230.0 - 245.9' greenstone 12.O - 245.9' - sulphides

9 50.0 - 90.0* - 0.05* Cu over 40.0*9 90.0 - 110.0* - 0.07* Cu over 20.0'9 150.0 - 195.0' - 0.05* Cu over 45.0'9 195.0 - 215.0* - 0.07* Cu over 20.0*

245.9 - 325.0* quartzitic arkose 245.9 - 275.0* - sulphides325.0 - 335.4* conglomerate335.4 - 390.2* arkose390.2 - 414.0* greenstone414.0 - 425.6* arkose425.6 - 467.0* greenstone

EOH

-AID-

Hole Jo.

69-1

0 - 5.0'5.0 - 950.0*

950.0 - 1071.7*

1071.7 - 1078.0'1078.0 - 2129.0'2129.0 - 2191.5*2191.5 - 2258.0'2258.0 - 2263.0*

2263.0 - 2651.0*

2651.0 - 2884.7'2884.7 - 2918.0*2918.0 - 2938.0*2938.0 - 3002.0

BOH

r — — — f —— j * — —

Location Bearing Dip

ci 106940 360 deg - 85 deg

overburdenfeldspathic quartzite; some sericitic seams,dlss pyquartzite, siliceous greywacke; scatteredargillite, chloriteargillite, volcanicbasalt; amygdaloidal, some py seamsbasalt w inter layered chloritic quzrtzitebasalt, scattered diss pyFAULT ZOVB; brecciated w 502 auartz-calcite at2259 - 2261*basalt; amygdaloidal w scattered chloriteseams, pybasalt, massive; broken coreFAULT ZOIE; breccia, mylonite, some felsitegabbro, felsitebasalt, diabase C?)

A. 4 Atlantic Ricltfleld Cmranv. 1908

Hole Jo.

P-2

075.0 - 172.0*172.0 - 250.0'250.0 - 268.0'268.0 - 300.0'300.0 - 325.0'325.0 - 2446.0*2446.0 - 2530.0*2530.0 - 4040.0'4040.0 - 4082.0'4082.0 - 4587.0*

BOH

Location Bearing Dip

ci 84020 90 deg

75.0* overburdenargillaceous greywackel imestoneargillitelimestonechloritic argillite, quartzitediabaselimestone, contortedgreywacke, quartziteargillitegreenstone, sheared siltstone

-All-

Hole Bo.____Location______Searing_______Dip

P-4 ci 86979 90 deg

O - 1595. O' log missing 1595.0 - 1675.0' diabase1675.0 - 1687.0* silty limestone, laminated1687.0 - 2350.0' silty argillite w pyrltlc sections; cherty 2350.0 - 2455.0* arkosic quartzite, cherty argillite; w

anhydrite2455.0 - 2525.0* diabase 2525.0 - 2625.0* arkosic quartzite2625.0 - 2850.0* arkosic quartzite w Interbedded argillite 2850.0 - 2962.0* quartzite

E O H

A. 5 Stanford Mines Limited. 1971-72

Hole 1: Dip -40 deg Depth 473 ft. Bearing Grid E

O — 14.O overburden14.0 - 215.5 arkose; foliated at 30 deg TGA.215.5 - 234.0 arkose, brecciated, faulted w hematite-filled

fractures234.0 - 242.7 diabase; some cp 242.7 - 273.0 arkose 273.0 - 278.0 Intermedlate-felslc tuff; sericltlzed; contacts at

25 deg TGA.278.0 - 378.8 arkose; scattered cp, hematite-filled fractures 378.8 — 385.6 arkose; fine grained sulphides, cp: some ehl

9 378.8 - 383.5* - 0.14* Cu over 4.7* 9 383.5 - 385.6* - 0.13* Cu over 2.1*

385.6 - 387.3 diabase; some cp-rich fractures

9 385.6 - 387.3* - 0.039* Cu over 1.7*

387.3 - 396.1 arkose; some cp

9 387.3 - 392.3* - 0.040* Cu over 5.0' 9 392.3 - 396.1* - 0.053* Cu over 3.8*

396.l — 405.O diabase; qtz-carb str, some cp

* 396.1 - 401.1* - 0.030* Cu over 5.0* 9 401.1 - 405.0* - 0.048* Cu over 3.9'

405.0 - 414.0 arkose; sil, chl w l* cp str, patches

-A12-

9 405.0 - 410.0' - 0.16* Cu over 5.0* 9 410.0 - 414.0' - 0.04* Cu over 4.0'

414.0 - 434.0 fault(?); strongly fractured w hematite and cpfilling; low Cu assays

434.0 - 473.0 arkose; some scattered cp EOH

9 444.0 - 449.0' - 0.049* Cu over 5.0'

Hole 2; Pip -50 deg Depth 242 ft. Bearing HV

O -14.0 overburden 14.0 -85.0 arkose; some cbl, cp 85.0 -89.0 diabase89.0 - 197.0 diabase, diorite; dlss py, cp at 100.0 - 121.0 197.0 - 242.0 arkose

EOH

- core split but not assayed

Hole 3; Dip -70 deg Depth 280 ft. Bearing 336 deg

O -12.0 overburden12.0 - 70.7 arkose; minor dlss cp w some chl70.7 - 72.0 magnetite-rich band; mlcaeous w qtz-carb str; some

cp In sil patches Clabelled Iron formation In log)

9 70.7 - 72.0* - 0.14* Cu, 0.25 oz Ag/T aver 1.3*

72.0 - 97.0 arkose; some specularite and py to base 97.0 - 262.7 diabase, diorite; carb str w py, CD and l* diss cp

at 173.3 - 175.5

9 173.3 - 175.5* - 0.94* Co, 0.14 oz Ag/T over 2.2*9 175.5 - 180.5* - 0.041* Cu, o. 10 oz Ag/T over 5.0'

262.7 - 280.0 arkose EOH

Hole 4; Dip -50 deg Depth 660 ft. Bearing TV

O — 36.O overburden36.O - 449.O arkose449.0 - 571.0 diorite (diabase?)571.0 - 607.6 volcanic C?) (possibly nipissing diabase); w

numerous fractures, str, masses of chalcopyrite;sil bx zone at 578.0 - 581.0

9 571.0 - 581.0' - 0.28* Cu over 10.0'9 571.0 - 574.0* - O 53* Cu over 3.0'9 584.0 - 605.0' - 0.41* Cu over 21.0'

-A13-

O 594.O - 595.0* - 1.12* Cnt 4.05 oz Au/T over l.O'

607.6 - 660.0 arkose EOH

Hole 5; Dip -70 deg Depth 876 ft. Bearing Grid V

034.0 -

515.0 -636.0 -641.0 -649.7 -658.0 -662.0 -809.0 -831.0 -843.0 -

Hole 6:

34.0515.0636.0

overburdenarkose; scattered qtz— carb str, cpdiabase

641.0 arkose649.7658.0662.0809.0831.0843.0876.0EOH

-

Diu

diabasearkosediabaseandesite tuff (?)greywackearkosegreywacke

no sampling or assaying indicated

-50 dear De nth 1.039 ft. Bearing Grid V

O — 46.O overburden46.0 - 594.0 arkose; w cp-bearIng qtz veining at 139.0

139.3, 149.0 - 149.2, 166.6 - 168.0.594.0 - 1,039.0 diabase, diorite, mafic volcanic<?)

EGH- no sampling or assaying indicated

APPEIDIZ B:

Dlaaond Drill Logs. Fort lioraan Explorations Inc., 1974

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9

APPETOIX C:

1968 Sock Sanple Descriptions and Analytical Kesnlts

United Beef Petrolenns Limited

ALDUS BOCK GBQCHEKISTKY RESULTS, 1988

Saaple Cn An Zn Pb Ag

390139023903390439083909391039113912391339143915391639173918392439253926392739283929393239333935393639383939394039433946394739513956395839593960396139623963396439653966396739683969 3973 3977

f 3978 398O

.011

.390

.225

.069

.016

.841

.45311.7766. 176.670

1.014.013.022.121LLLLLLLLL

.113

.021LLLLL

.030L

.044

.020

.037

.014

.022LL

.022

.046

.022

.011LL

.022L

.010L

82266231419

1588914842379132811

3511011104899571641799

1668528L

12615L1564519878

167L76613

LLLL

.010LLLLLLLLLL

.020

.026

.028

.024

.013

.010

.013

.017LL

.020

.014

.010L

.015

.015

.012LLLLL

.017

.025

.021L

.076

.110

.402

.038

.012

.026

.014

.032

LLLLLLLLLLLLLLLLLLLLLLLLLLLLL

.016LLLLLLLLLLLL

.012

.015LLLLL

LLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLLL

3981 L 10 .034 L L3982 .418 16 L L L3983 .319 16 L L L3993 . 061 6 L L L4001 .039 L L L L4002 .018 6 L L L4003 .024 6 L L L4008 .658 209 L 1.396 294009 .226 724 L .073 34010 .103 351 L .932 184011 .222 1889 L .856 77

BUCK DESCRIPTIONS FOR A1OHALOUS SAMPLES. 1988(most sample sites given on 1994 geology sheets, detailed

sampling not shown)

Sample Location Assay

3901 L16+90V, 26+901 O.Oil* Cu in grab

— 2—foot wide chlorite schist, qtz vein zone with some pink calcite and barite; with chalcopyrite, chalcocite and malachite; cross—cut by epidote veinlng.- localized along the trace of the Flack Lake Fault (mylonite) in Gordon Lake Fm sandstone.

Sample Location Assay

3902 L16+90V, 26+905 O.3901 Cu over 2.0 ft.

- as 3901, a 2-foot wide sample across qtz vein-chlorite schist zone; vein pinches and swells.

Sample Location Assay

3903 L16+90V, 26+901 Q.225% Cu over 1.0 ft.

— as 3901, a 1-foot wide sample across qtz vein—chlorite schist.

Sample Location Assay

3904 L6+20E, 3+5 O IT 0.069* Cu in grab

— grab sample of malachite—bearing brecciated carbonate (albite?-?.O. V. ) debris, probably from nearby trench.- along the trend of the Vo. l Copper-Precious Metal Structure mapped during the 1993-1994 progre

Sample Location Assay

3908 L17+90E, approx TL10+OOV 0.016* Cu In grab

- sample of carbonate veInlets In chlorite schist of an oblique shear zone to the To. l Copper-Precious Metal Structure; also in area of sample 9420.- host rock is Espanola Fm dolomite.- irregular, anas tom! z ing carbonate -i-/— hematite veinlets trend 082/55S with some chalcopyrlte-bearlng carbonate */- quartz tension veinlets at 110/74S; some hematite, silica and chlorite alteration.

Sample Location Assay

3909 Main Showing, O.841* Cu over 5 ft. south face of Main Pit

-chip channel across chlorite schist (068/708) with some oblique quartz veinlets and containing l* chalcopyrite, 2* pyrite; some silicification and chloritization.

Sample Location Assay

3910 as 3909 O.453* Cu, 0.005 oz Au/T over 5 ft.

- chip channel as 3909 with 3-4* chalcopyrite along schistosity planes.

Sample Location Assay

3911 as 3909 11.776* Cu, 0.026 oz Au/T over 6.5 ft.

- chip channel as 3909 with abundant chalcopyrite stringers subparallel to schistosity.

Sample Location Assay

3912 as 3909 6.176* Cu, 0.014 oz Au/T over 6.5 ft.

- chip channel across sulphides as knots (clots) within quartz veins; 8* chalcopyrite, l* malachite, 3-5* pyrite, trace chalcocite; some carbonate In veinlng.

3909 — 3912, a continuous sample Interval; avg grade 5.35* Cu over 23 ft. with a 13-foot section of 8.981 Cu, 0.02O oz Au/T.

Sample Location Assay

3913 Main Showing,small pit 0.6702 Cu over 3.3 ft. 10 ft. east of Main Pit

- chip channel across quartz tvein)-rich zone.

Saaple Location Assay

3914 as 3913 1.0141 Cu over 3.3 ft.

— chip channel across quartz tvein)-rich zone.

iles 3913 - 3914, a continuous sample Interval; avg grade O.8422 Ga aver 6.6 ft.

Sample Location Assay

3915 L6+70E, approx TL10+OOF 0.0131 Cu in a grab

- grab sample of malachite-bearing quartz-carbonate-veined and schistose Espanola Fm feldspathic sandstone debris in an old trench.- along the trace of the So. l Copper-Precious Metal Structure.

Sample Location Assay

3916 L1+40V, approx TL10+OOH O.022* Cu in a grab

- dissem pyrite, traces chalcopyrite in silicified Espanola Fm quartzitic—feldspathic siltstone, limestone; close to sample 9406A.- along the trace of the to. l Copper-Precious Metal Structure and Trench Tla ^993).

Sample Location Assay

3917 as 3916 O. 121* Cu in a grab

- < 2% pyrite, malachite parallel bedding, Espanola Fm siltstone; silicified, chloritized; in part chlorite schist.

Sample Location Assay

3918 L4+80V, 2+001 351 ppb gold in a grab

- quartz veinlets at 255/42F, 052/78S in Espanola Fm feldspathic sandstone (siltsone?); traces of pyrite, malachite.- localized along the trace of a F-ME trending fault structure C1994 mapping/interpretation).

Sample Locat ion Assay

3924 L19+OOV, 10+801 0.0202 Zn in a grab

- 3X dissem pyrite localized along bedding in Espanola Fm siltstone/chert; So = 295/18S.

Sample Location Assay

3925 L22+50V, 10+605 0.0261 Zn in a grab

- traces of pyrite in Espanola Fm siItstone/sandstone; ripple marks; SO ^ 220/74V.- close to Scarbo Creek; a fault zone?

Location Assay

L17+OOV, 5+30S 0.028* Zn in a grab

- traces of pyrite and carbonate velnlets in Espanola Fm siltstone/chert; So = 058/15S, SI s 105/88S (fracture cleavage?) and carbonate veinlet orientation at 042/90.- localized along the trace of a HV-SE trending fault, along Scarbo Creek.

Sample Location Assay

3927 L15+OOV, 1+001 O.024* Zn in a grab

- weakly pyrltlc quartz veinlets parallel bedding in Espanola Fm laminated siItstone/sandstone; So - 292/90.- in the vicinity of the axial trace of the Little White River Anticline.

Sample Location Assay

3928 as 3927 0.013* Zn in a grab

-quartz—carbonate blebs and Irregular stringers in Espanola Fm siltstone with dissem pyrite; locally silicified, hematltized and chloritlzed.

Sample Location Assay

3929 L14+80V, 0+8OF 0.010* Zn in a grab

- pyrite and irregular quartz veining, breccia in Espanola Fm dolomite, limestone; very close to 3927, 3928.

Sample Location Assay

3932 L16+2OV, 26+905 O.013* Zn In a grab

- shear zone flanked by crush breccia In Espanola Fm siltstone, adjacent the Flack Lake Fault; schistosity at 064/65S; variably hematltlzed.

Location Assay

L16+40V, 26+905 0.017* Zn In a grab

- shear zone trending 070/10S with quartz velnlets and dlssem pyrite hasted by Espanola Fm siltstone adjacent to the Flack Lake Fault; some silicification.

Sample Location Assay

3935 L16+50V, 3+505 0.113* Cu In a grab

- brecciated, bedded Espanola Fm limestone-dolomite with some pyrite, chalcopyrite in breccia and quartz velnlng subparallel to bedding.- outcrop along Scarbo Creek and proximal to the Little Vhlte Siver Anticline axial trace.

Sample Location Assay

3936 as above 0.02li Cu in a grab

- similar to 3935, with l* pyrite, more quartz velnlng and chloritization.

Sample Location Assay

3937 L16+70V, 3+905 0.020Z Zn over 6 ft.

- series of grabs quartz-chlorlte breccia zone in Espanola Fm limestone- dolomite; zone oriented 114/90 with pyrite in host.

Sample Location Assay

3938 as above 0.014* Zn over 9 ft.

- similar to 3937, a series of grabs over 9 ft.

Sample Location Assay

3939 as above 0.010* Zn over 5 ft.

- similar to 3937, a series of grabs over 5 ft.

Sample Locat ion Assay

3943 L41+OOE, 23+OOff 166 ppb Au in a grab

- sericitized, hematitized Mississagl Fm feldspathic sandstone.; some quartz pebble horizons.

Sample Location Assay

3946 L40+OOE, 25+003 0.016* Pb. 0.015* Zn in a grab

- bedding parallel quartz veinlets at 072/28S in silicified Espanola Fm limestone/siltstone; veinlets more or less at contact.

Sample Location Assay

3947 L39+80E, 1+2OS 0.0302 Cu, 0.0151 Zn in a grab

- 6" quartz vein plus veinlets at 276/699 in Nipissing gabbro. Close to a northeasterly fault trace.

Sample Locat ion Assay

3951 L44+OOE, 11+30S 0.012* Zn in a grab

- pyrrhotite-pyrite-bearing Nipissing diabase, epldotlzed; close to an east-west fault trace.

Sample Location Assay

3956 L32+OOE, l1+8OF O.044* Cu, 126 ppb Au in a grab

- vuggy quartz vein with chlorite selvedges (quartz-chlorite breccia - J.Q.V.) in Espanola Fm dolomite; close to Main Showing and a WE fault trace.

Sample Location Assay

3958 L33+80E, 13+10E 0.020* Cu in a grab

- pyrite, chalcopyrlte-bearlng Irregular quartz-carbonate veinlng in Espanola Fm limestone/siltstone. In creek bed east of Main Showing.

Sample Location Assay

3959 as above 0.037* Cu over 2 ft.

- 2—foot chip channel over a quartz pod/vein which shows boudinage along 090/45S in chlorite schist; contains pyrite and chalcopyrite.

Sample Location

3960 as above O.0141 Cu in a grab

- quartz veinlets and chlorite selvedges containing chalcopyrite and pyrite in Espanola Fm limestone/siltstone.Sample Location

3961 L32+80E, 11+90V 0.022* Cu over 4 ft.- 4-foot chip channel sample across chlorite schist containing numerous quartz pods with pyrite, chalcopyrite; some hematltization; sample from North Pit, Main Showing area.

Sample Location Assay

3962 L28+OOE, 5+805 0.017* Zn in a grab

- brecciated Espanola Fm limestone in contact with Nipissing diabase. Possibly along the trace of an E1E fault.

Sample Location Assay

3963 L28+20E, 3+8OF O. 025* Zn In a. grab

- pyritic Flpissing gabbro close to a FBTE fault trace. Sample Location Assay

3964 L23+80E, 5+8Off 0.022ZCu, O.021* Zn in a grab- silicified Espanola Fm limestone with traces pyrite at the contact with Nipissing diabase.

Sample Location Assay

3965 L22+OOE, 9+25* 0.046* Cu in a grab

- zone of chlorite schist (TSS- see '94 legend) In Espanola Fm dolomite.

Sample Location Assay

3966 L19+40E, 9+60J 0.022* Cu, 0.076* Zn in a grab- quartz-veined frost heave of chlorite schist tfSS) in Espanola Fm dolomite. Also close to a VE fault trace.

Sample Location Assay

3967 as above O.0102 Cu, O.1101 Zn In a grab

- as 3966.

Sample Location Assay

3968 L15+05E, 8+30H 0. 015* Pb, 0.402* Zn in a grab- chlorite schist (TSS?) containing 40-60* quartz velnlng plus carbonate and pyrite.

Sample Location Assay

3969 as above O.038* Zn in a grab

- as 3968.

Sample Location Assay

3973 L16+OOE, 10+15F 0.022* Cu, 0.012* Zn in a grab

- fracture zone at 014/35S containing some carbonate, malachite, chalcopyrite and pyrite in a narrow diabase sill; local hematitlzation.

Location Assay

L7+80E, 5+90H 0.026* Cu in a grab

- frost heave of Vipisslng diabase in contact with Espanola Fm limestone; limestone is brecciated and quartz—veined; contact is chloritized and mineralized with 1-2* pyrite.

Sample Location

3978 as above 0.010* Cu, 0.014* Zn in a grab

- as 3977.

Sample Location Assay

3980 L8+OOE, 9+55IT 0.032* Zn in a grab

- frost heave Espanola Fm quartziteXsiItstone containing quartz-carbonate stockwork and 1-2* pyrite.

Location Assay

L7+10E, 9+455 0.034* Zn in a grab

- irregular quartz velnlets to 3 cm wide at 285/90 within Espanola Fm limestone/dolomite; close to a V-S fault trace.

Sample Location Assay

3982 L32+40E, 12+001 0.418* Cu in a grab

- quartz vein boulder containing malachite, chalcopyrite in the vicinity of the Forth Pit, Main Showing area.

Sample Location Assay

3983 L32+50E, 12+75V O. 319* Cu in a grab

- chlorite schist with chalcopyrite, malachite; pit debris from the Ka In Showing area.

Sample Location Assay

3993 LO+00, 4+85V O. 061* Cu in a grab

- Espanola Fm C?) feldspathic sandstone containing 15* pyrite and traces malachite, chalcopyrite; proximal to Nipissing diabase.

Sample Location Assay

4001 L10+OOV, 16+20V 0.039* Cu in grab

- pyrite, malachite in chloritic shear zone within Espanola Fm dolomite/siltstone; sample from a pit.

Sample Location Assay

4002 as above 0.018* Cu In a grab

- as 4001.

Sample Location Assay

4003 as above O . 024* Cu in a grab

- as 4001.

Sample Locat ion Assay

4008 somewhere south of 1.396* Pb, 0.658* Cu, 209 ppb Au the property in a grab

- 3.5— foot wide quartz vein at 022/64S in feldspathlzed Nipissing diabase containing 3-5* chalcopyrite, 5-7* galena, 1-2* specularite, 1-2* sphlerlte, some arsenopyrite and chlorite selvadges; fractured at 063/72S, 131/80S and 181/76S?

Sample Location

4009 as above 0.226* Cu, O.073* Pb, 724 ppb Auin a grab

- 2-foot wide quartz vein at 353/55V; similar mineralization and host to 4008.

Location Assay

4010 as above 0.932* Pb, 0.103* Cu, 351 ppb Auin a grab

- quartz flooding zone in a chloritic shear within Tlpissing diabase.

Sample Location Assay

4011 as above 0.856* Pb, 0.222* Cu, 1889 ppb Au(0.06 oz Au/T) in a grab

- gossan-bearing shear zone in nipissing diabase with traces at arsenopyrite.

AFPEMDIX D:

1993 Rock Saaqrte Descriptions and Analytical Basalts

1993 RAMPT.K *wp *T*T.YTTC*T, CJnl —4)

Sanple

294201294202294203294204294205294206294207294208294209294210294211294212294213294214294215294216294217294218294219294220294221294222294223

Location Type

L2+OOV,L2+OOV,L2+OOV,L1+50V,L1+50V,L2+OOB,L2+OOE,Ll+OOE,Ll+OOB,Ll+OOE,L3+OOE,Lll+OOBL7+50E,main showingHVT 546 szL20+OOE, 11+OOHmain T pitnain V pitmain F piteast of F piteast of F pitmain S pitnaln SV pit

TL10+OOF TL10+001 TL10+OOF TL10+OOF TL10+OOF TL10+OOF TLl0+0OF TL10+OOF TLl0+0OF TL10+OOF TL10+OOF TL10+OOF

TL10+OOF

grabgrabgrabgrabgrabgrabgrabgrabgrabgrabgrabgrabgrabgrabgrabgrab

In chip-south 1m chip-centre In chip-north grab-north end grab-south end

grabgrab

Metallic Analytical

- part of a 33-element ICP package- Cu, VI, Co, As, Ag, Zn as ppn.- Fe as 3*.- Au as ppb.

Sample Cn

294201294202294203294204294205294206294207294208294209294210294211294212294213294214294215

2,6196, 148

MO, 000MO, 0003,092535169392013141214

MO, 000683

13128

117

18176

24111524165419

Co Fe As Zn

885899

1171398

2515399

1.511.191.601.830.742.402.763.213.762.511.002.211.65

M5.004.87

266468

10810126

3618406

62

422214141020146128

13012

4045

10

110

0.40.82.01.40.8

40. 2^0. 20.4

^0. 2^0. 20.2

•CO.20.2

26.03.6

Metallic Assays

- Cu, Vi, Co, Fe, As as H , fusian-ICP-AES- S as *, Leco IR Detector- Au as ppb, FA-AAS- Ag as ppjn, AAS-BKGD CORE- Au*, Pd, Pt (not shown) as ppb, FA-ICP-AFSSaaple Cu Vi Co Fe As S Au Ag294203 1.26 ^. 02 410.01 1.8 ^.01 1.18 22*294204 0.88 -CO. 02 ^.01 2.1 W . 01 0.78294214 18.10 ^.02 <0.01 21.5 <0.01 18.20 112*294217294218294219294220294221294222

294217294218294222

2.885.300.560.060.024.64

^.02 '<0. 02 ^{ 0 . 02 *<0. 02 *<0.02 x<0. 02 x

:o.oiCO. 01:o.oiCO. 01:o.oiCO. 01

5.09.45.71.31.38.0

^.01<0. 01<0. 01"10. 01^.01<0.01

2.595.460.470.060.034.68

5080^^<575

74*100*120*

4.28.20.6

<0.2•^. 25.0

APPEIDIZ E:

1994 Sock Sample Descriptions and Analytical Kesults

Sample Ho. Location Description

9401 L2+OOV TLl0+0ON -chip sample over 4 ft., East Face; East Rx Face chlorite alteration zone plus albite Trench l alteration zone, south side of face.

-3-51 malachite in all sections with 22 cp, 12 py in quartz stringers in chlorite zone and up to 12 cp-fllled fractures in albite zone.

9402 " -chip sample over 6 ft.; quartz-albitealteration and breccia zone with 32 quartz—carbonate velning.-32 cp, some py as pods and blebs in all phases; some as inclusions in chlorite patches; 12 malachite.

9403 " -chip sample over 5 ft.; quartz-albitebreccia and alteration zone w up to 102 quartz stringers, veinlets.-12 cp, 22 py blebs and Irregular masses mainly associated w quartz +S- Fe-carb velning; 32 malachite throughout.

9404 " -grab sample; albite-slllca alteration w102 quartz velning.-32 cp blebs and 102 malachite.

9405 " -chip sample over 6 ft.; chlorite-quartz+S- albite breccia and alteration zone C152) in host siltstone.-cut by narrow quartz-chlorite veins which contain some large splashes of cp; local silicification to l" in vein host.-some malachite, hemitlte in host rock.

9406 " -chip sample over 3ft; quartz-chloritebreccia with some late quartz velning.-several small grains of cp in quartz and albite plus scattered malachite.

9406a Ll+OOV TL10+OOH -chip sample over 5 ft.; sillca-alblte Trench 1A alteration zone w minor bs; some later V9402 quartz-carbonate velning (12); sample

contains some host rock, apparentlysiltstone.-3-52 cp blebs mainly in siliceous sections some of which may be late, and 72 malachite.

9407 L2+OOV TL10+OOF -a representative grab sample covering East Bx Face the Interval 1-10 ft. across the top of

Trench l the Bast Rock Face; consists of albite alteration zone.

9408

9409

9410

-chip sample over 10 ft. across top of face, Interval 10-20 ft.; consists of albite alteration zone with 102 quartz- carbonate veining, stringers; some silicification?-3-52 irregularily distributed masses of cp, traces py and a few grains of aspy.-82 malachite, minor azurite.-includes some calcareous sediment (siltstone?).

-chip sample over 10 ft, across top of face, Interval 20-30 ft.; quartz-albite breccia and extensive albite alteration zone; some relict host rock laminations.-52 quartz, 22 cp blebs and masses, 52 malachite.

-chip sample over 10 ft., across top of face, Interval 30-40 ft.; quartz-albite alteration and breccia zone with 32 malachite staining.

9411

9412 Ll+OOV 9+80V

-chip sample over 10 ft. across top of face, interval 40-50 ft.; consists of albite (bx) alteration w 12 malachite, quartz-chlorite breccia w 32 Irregular masses and dlssem cp, plus some host limestone.-cp mainly contained in quartz.

-grab sample; albite and chlorite alteration zone w 22 quartz -l-/- carbonate veining In host calcareous siltstone and limestone.-32 cp as blebs and stringers, minor py and 52 malachite.

9413 Ll+OOE TLIO+OOF Trench 2, East Face

-chip sample over 4 ft., interval 21-25 ft.; mixed zone of cuartz-Fe—carbonate- chlorite breccia and chlorite (alteration?); some vuggy aspect to breccia.

9414

9415

9416

9417

-chip sample aver 8 ft., interval 25-33 ft. and Including 5 ft. of cover; quartz- carbonate-chlorlte breccia w some later quartz stringers; tr cp.

-chip sample over 8 ft. , interval. 42-50 ft.; quartz ^/-carbonate)-chlorite breccia.

-chip sample over 5 ft., Interval 50—55 ft.; quartz-carbonate veining and breccia in intensely sheared green calcareous sediment or chlorltlzed limestone.-201 vein material; one 1/4" vein contains 451 cp, SK malachite.

-chip sample over 5 ft., Interval 55-60 ft.; mainly light brown to buff weathered, light grey limestone with some 8" of quartz (carb)-chlorite breccia.

9418 L2+OOE, 10+OON -Chip sample over 5 ft; narrow (-CI ft.)quartz vein in quartz-(chlorite) breccia. -10* malachite w 1-2* cp +X- py as large (1/2" dia) blebs and some dissem; mainly contained in quartz vein material, possibly post-breccia.

9419 Lll+OOE TL10+OON -grab sample from a small trench;chlorite-quartz-albite breccia; no

W9404 visible mineralization.

9420 L17+OOE TLlO+OOff -grab sample; talc-chlorlte (actinolite)schist and chlorite breccia with

V9406, 9409 stringers of quartz; 5* chlorite clotsor frags, a few albite frags.

9421 L27+OOB 10+OOH -grab sample of dolomitic limestone;pale greenish grey, weathers buff to

V9413 light brown; totally crystalline w somevery thin darker laminae; no visible mineralization.

9422 L31+30B 15+90S -chip sample over 8 ft.; mainlyMain Showing mineralized quartz-chlorite breccia w

Pit l some massive sulphide pods and a few bands of semi-massive py—cp parallel altered host rock laminations.-15* cp w some bn, py in vein material.-overall this sample 45* sulphides of which 20* is cp; 3-5* malachite.

9423 " -chip sample over 9 ft.; mainly chloriticshear w quartz stringers and large semi- massive cp-py pods; also 50* quartz- chlorite breccia and quartz-carbonate veinlng containing cp blebs and stringers; some vein material parallel to host rock laminations; siltstone?-overall sulphide content this sample, 8* cp w minor py, tr bn plus 5* malachite.

9424 " -chip sample over 6 ft; quartz vein/sllalte zone; some vuggy quartz vein material; most of veinlng is late; also chlorlte-quartz breccia.-a few massive py-cp pods w tr bn in chl material; < l% dissem cp in late veins; 3* malachite throughout.

9425 " -chip sample over 9 ft.; quartz veIn/silalteration zone; up to 50* vuggy qtz vein material w strong sil of laminated sed Climestone or siltstone); some qtz-chl bx.- 3* pyrite w scattered associated cp, all as massive pods to 4" dia and blebs in qtz; 8* malachite in vein and host; some albite as alte and frags.

9426 L40+OOV 3+OOS -grab sample; fine grained calcareoussiltstone, pale light greenish grey,

V9413 weathers brown to light grey; weaklaminations or schistosity and a z— crenulation fabric.- l* dissem py.

9427 L28+OOV 7+OOS -grab sample; narrow quartz stringers^*) in schistose siltstone; tr py.

9428 L12+OOW 12+OOS -grab sample; fine-medium grainedquartzitic sandstone-siItstone with5* flecks of orange weathered feldspar;35* Quartz, tr pyrite; somewhat sil C?).

9429 L6+OOV 12+5OS

9430 L49+OOV 3+80S

9431 L48+50V 3+8OS

9432 L48+OOV 3+50S

9433 L40+OOV 3+5OS

9434

9435

L36+OOV 5+OOS

V9423

L32+OOV 4+0 OS

V9424

-grab sample; narrow quartz vein In weakly sheared and chl silts-cone; 201 of sample consists of quartz vein material.

-grab sample; Irregular quartz stringer zone-stockwork In silicified pinkish feldspathic quartzite; some quartz flooding or reconstitution of quartzite component.-some narrow quartz veinlets showing preferential east-west attitude.-no visible sulphide mineralization.

-grab sample; mixed quartz velnlng and chloritic shear zone material hosted by feldspathic quartzite; trend is oblique to stratigraphy.-21 py in chlorite shear.

-chip sample over 3.2 ft; massive white quartz vein in feldspathic quartzite; tr py or cp.

-grab sample; weakly-moderately chl quartzose siltstone Cup to 102 quartz grains).-several narrow quartz veins/stringers Cto 1071) containing 32 cp, seme py; also some hematite, malachite and azurite. Albite?; 1-2* dissent, splashes cp in siliceous pods, strings; local silicification of host.

-grab sample; quartzitic to arkosic sandstone/siItstone, light grey.-lit quartz ve inlets w scattered cp

*s, dissem (32) plus traces py.

-grab sample; quartz—ankerite veining in chl, weakly sil siltstone.—32 Irregular blebs and masses of chalcopyrite; 1-22 malachite; traces of hematite and pyrite.

9436 L18+OOV 18+OOS -grab sample; white bull quartz w 102feldspar fragments and 52 chlorite fragments or assimilated host conglomerate . -no visible mineralization.

9436a L32+OOV 2+30S

V9425

-grab sample; chloritlzed, weakly albltlzed sheared and somewhat brecciated to vuggy siltstone.-w 2-53 narrow schistosity parallel quartz -l-/- feldspar veins.-situated at the northern edge of a quartz-alblte—chlorite breccia zone.

9437 L12+OOV 4+OOS

9438 L24+OOV 6+70S

-grab sample; moderately sil, chl grey green quartzitic sandstone.-2-31 cp, py masses and some scattered dlssem, 21 malachite.-some narrow py-cp-fllled fractures.

-grab sample; dark green, strongly magnetic rock, possibly intrusive. Vith 10*, <l/Qtt dla subangular translucent quartz grains.-minor quartz-carb veinlng.

9439 L4+30V, 5+OOS

9440 L3+50V, 4+60S SE Trench

9441 L3+50V, 4+6OS SE Trench

-grab sample of l foot wide chl-gossan shear zone in arkosic sandstone/ conglomerate; contains l" wide quartz vein (103 of sample) which contains 23 dlssem cp, 103 malachite.

-chip sample over 5 ft.; quartz-Fe—carbvein and stringer zone in sheared,weakly chl conglomerate/sandstone; veinmaterial comprises 253 of sample, ofwhich 303 is Fe-carb.^13 dlssem cp in quartz, some malachitestaining.

-chip sample over 4 ft.; sulphide-rich quartz-Fe-carb veinlng and some str in sheared conglomerate; main vein to 3 ft. wide; extensive gossan in host, minor bx.-53 Fe-carb.-253 semi-massive patches of cp, gn, py, generally as isolated groups, all In vein material; py very bright and some may be gn; some aspy?; cp as amorphous massives to anhedral crystalline w some copper reddish tarnishing; 2-53 emerald green malachite In both velning and host rock.

9442 L3+35V, 4+6OS SE Trench

9443 L5+OOY, 4+50S

-chip sample over 6 ft. of mineralized quartz vein from trench, 15 ft. to east of 9441; also contains 101 cbl host rock material.-mainly white quartz w some scattered Fe- carb-filled vugs; 101 cp and py or gn masses, very unevenly distributed; some barren patches of quartz velnlng.-minor malachite.

-grab sample of vuggy quartz vein float material from a trench on strike with SB Trench; strong gossan and 15X cp and dissem; host is conglomerate.

CESTIPICATES OF ANALYSIS

Che

mex

Lab

s Lt

d,An

alytic

al Ch

arnia

n * Q

aoch

wnM

a' Ra

gMar

ad A

tMya

re61

7STi

mbM

tM B

lvd.,

Mlss

laaau

ga,

Ont

ario

. Can

ada

L4W

2S3

PHO

NE: 9

06-6

24-2

806

lo:

N R

S, J

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E AS

SOCI

ATES

LIM

ITED

2603

HO

LLIN

QTO

N CR

ES.

MIS

SISS

AUQ

A, O

N LS

K 1E

6

Com

nwnt

o:

ATTN

: JOH

N M.

SIR

IUNA

S

A931

7646

CERT

IFIC

ATE

A931

7646

N R

A J

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ASS

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ATES

LIM

ITED

Prol

tot:

JENT

INA

P.O.

#:

•am

plea

aut

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ad t

o m

ix l

ab i

n H

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ga,

Thl

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port

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en

H-A

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OH.

SAM

PLE

PREP

ARAT

ION

W20

122

4 aa*

sm IS

IB

IS

1l

DESC

RIPT

ION

Aaa

ay r

ing

to a

ppro

x IS

O me

ah

0-5

Ib o

ruah

and

apl

it

ICP

- AQ

Dig

aatio

n ch

arge

The

3a e

lement Z

CP package i

* au

itab

le fer

trace

meta

la

in

aeil a

nd reek a

amplea.

Blemwta

fer

whie

h the ni

trio

-aqu

a regia

digestion

ia pee

aibl

y in

oomp

lete

are

i Al,

Ba,

Be,

ea,

Cr.

Ga,

K, La,

Mg,

Ha,

Ir,

Ti,

TI,

H.

ANAL

YTIC

AL P

ROCE

DURE

S

CHEM

EXCO

DE 100

2118

an*

aiao

aiai

2122

2123

21

2421

21a ia

c21

27ai

aia le

o31

3021

3121

3221

S121

3421

3521

3621

37ai

ai21

3*21

4031

4131

4321

4331

4421

4531

4C31

4731

4131

49

NUMB

ERSA

MPLE

S

IB IS IB IB IB IB IS

IS IS IB IS IS IS IS IB IB IS IS IS IS IS IB IB IB IS IS IS IB IS IS IS IS IB

DESC

RIPT

ION

Au p

pbi

ruae

10

g aa

mpl

eAg

ppm

i 33

ele

aMat

, ae

il A

roo

kA

l tit

33

elaa

wnt

, ae

il f

t re

ekAa

PPM

I 33

ele

men

t, ae

il f

t re

ekBa

PPM

I 33

ele

men

t, ae

il f

t re

ekBe

ppM

i 32

ele

men

t, ae

il f

t re

ekBi

PPM

I 33

ele

men

t, ae

il f

t re

ek

Ca t

ii 33

ele

men

t, ae

il f

t re

ekCd

PPM

I 33

ele

men

t, ae

il f

t re

ekCo

PPM

I 33

ele

men

t, ae

il f

t re

ekCr

ppM

i 33

ele

men

t, ae

il f

t re

ekCu

PPM

I 33

ele

men

t, ao

il f

t re

ekre

tit

33 e

lem

ent,

aoil

ft

reek

aa p

pMi

33 e

lem

ent,

veil

ft

reek

Hg P

PMI

33 e

lem

ent,

aoil

ft

reek

K *i

33

elem

ent,

aeil

ft

reek

La P

PMI

33 e

lem

ent,

aeil

ft

reek

Mg t

it 33

ele

men

t, ae

il f

t re

ekMn

ppm

i 33

ele

men

t, ae

il f

t re

ekale

PPM

I 33

ele

men

t, ae

il f

t re

ekHa

Hi

33 e

lem

ent,

aoil

ft

reek

Hi

ppm

i 33

ele

men

t, ae

il f

t re

ekP

PPM

I 33

ele

men

t, ae

il f

t re

ekPb

PPM

I 33

ele

men

t, ae

il f

t re

ekflb

ppm

i 33

ele

men

t, ae

il f

t re

ek•o

ppm

i 33

ele

men

t a,

aeil

ft

reek

•r p

pmi

33 e

lem

ent,

aeil

ft

reek

Ti H

i 33

ele

men

t, ao

il f

t re

ekTl

ppm

i 33

ele

men

t, ae

il f

t re

ekU

ppm

i 33

ele

men

t, ao

il f

t re

ekV

ppm

i 33

ele

men

t, ao

il f

t re

ekW

PPM

I 33

ele

men

t, ae

il f

t re

ekIn

ppm

i 33

ele

men

t, ao

il f

t ro

ek

METH

OD

FA-A

Afl

XCP

-ABf

ICP-

AU

ICP-

AB

flIC

P-A

UIC

P-A

Bfl

ICP

-AII

IC

P-A

Bfl

ICP-

AB

fIC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

AB

fll I

CP-A

Bfl

( IC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

AB

flIC

P-A

Bfl

ICP-

ABf

lIC

P-A

Bfl

ICP-

ABf

lIC

P-A

Bfl

DETE

CTIO

NLIM

IT B0.

30.

013 10 0. 0.

0 0. 0.01 10 1

0.01 10

0.01

s 10.

011 10 3 3 1 1

0.01 10 10 1 10 3

UPPE

RLIM

IT

1000

030

0IB

. 00

1000

010

000

100.

010

000

IB. 0

010

0.0

1000

010

000

1000

0IS

. 00

1000

010

000

10.0

010

000

IS. 0

010

000

1000

0S.

00

1000

010

000

1000

010

000

1000

010

000

S. 0

010

000

1000

010

000

1000

010

000

Che

mex

Lab

s Lt

d,An

alytic

al Ch

tmM

*- Qa

oche

mM* *

R*g

l* 61

75 T

imba

rtaa

Blvd

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aalsa

auga

, On

tario

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ada

UW

2S3

PHON

E: 9

06-6

24-2

806

To:

N R

4 J

RESO

URCE

ASS

OCIA

TES

LIM

ITED

2803

HOLL

INQ

TONC

RE8.

M

ISSI

SSAU

QA.O

N L6

K1E6

Proj

ect:

JENT

INA

Com

men

t*:

ATTN

: JOH

N M.

SIR

IUNA

S

Pag*

Num

ber

:1-A

To

tal P

ag**

:l

C*r

tiflo

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ato:

29^U

L.93

In

voice

No.

: 193

1764

6 P.

O. N

umbe

r :

Acco

unt

:IEB

SAMPLE

194301^

194303^

194303V

1943

04

1943

0S

'

I9430C .S

1943

07 ^

1943

08 v/^

194309 vX

1943

10 v

1943

11^

1943

13 -

194313 -^

1943

14 "^

1943

1S

ra ea 301

301

308

308

308

308

308

308

308

308

308

308

308

308

308

IV DI 33 C

33(

336

336

336

336

336

336

336

336

336

336

336

336

336

AU p

pb

Ag

Al

AS

Bl

BeIA+AA

ppn

* PPB

ppB

ppi

< t

0.

0.88

10

0.

< B

0.

0.33

<

10

0.

40

3.

0.34

10

0.

45

1.

0.56

10

0.

< B

0.

0.33

10

0.

4 S

< Q.

1 .

30

8 10

0.

< B

< 0.

1.

44

10

10

0.

< B

0.

0.73

8

10

0.

< B

< 0

. 3.

13

10

10

0.

< B

< 0.

1.

37

13

10

0.

4 S

0.

0.4B

6 10

0.

10

4 0.

1.

13

36

10

0.

4 S

0.

0.94

18

10

0.

110

36.0

3.11

40

10

4 0.

4

B 3.6

0.90

6 BO

4

0.

CERTIFICATE OF ANALYSIS

Bi

Ga

Cd

Co

Gr

Ga

r*

Ot

1PP

B \

PPI

PPB

PPB

PPB

* PP

B Pi

0.17

0.

301

3630

.5

1 4

10

0.09

0.

386

61SO

.19

4 10

4 O.

B8

0.

318 ^0

000

.60

4 10

0.06

0.

346

xlOO

OO

.83

4 10

0.4B

0.

333

3090

.74

10

4 0.

39

0.

9 391

S3S

.40

4 10

4 1.

31

0.

11

334

169

.76

10

m. 00

0.

7 31

39

.31

4 10

3.53

0.

13

333

30

.76

10

3.B3

0.

9

16S

13

.SI

4 10

0.64

0.

8 251

14

.00

4 10

O.B9

0.

25

393

13

.31

4 10

O.S3

0.

IS

186

14

.69

10

0.06

0.

39

70 t

lOOO

O X1

5.00

4

10

13. SO

0.

9 39

683

4.87

4 10

A931

7646

lg K

La

Hj

Mn

p *

PPB

* ppB

0.11

10

0.

73

130

0.03

10

0.

17

95

0.13

10

0.07

105

0.08

10

0.

44

65

0.03

30

0.13

130

4 0.

01

10

1.10

340

4 0.

01

10

1.34

4SS

4 0.

01

4 10

3.66

6900

0.01

4

10

1.91

6SO

4 0.

01

4 10

1.43

10SO

0.01

10

0.43

355

0.03

4 10

0.91

350

0.01

10

0.89

380

0.03

10

3.30

300

0.30

4

10

3.69

1115

CERT

IFIC

ATIO

N:.

Che

mex

Lab

s Lt

d,An

alytic

al Ch

emto

lt * Q

eooh

tmMi

* Re

gMer

ed A

tMye

ra51

76 T

lmba

riaa

Blvd

., M

iaat

oaug

a,

Onta

rio, C

anad

a L4

W2S

3 PH

ONE:

906

-624

-280

6

To:

NR

& J

RESO

URCE

ASS

OCIA

TES

LIM

ITED

2803

HOL

LINQ

TON

ORES

. M

ISSI

SSAU

QA.O

N L6

K 1E

8Pr

ojec

t: JE

NTIN

ACo

mm

ents:

AT

TN: J

OHN

M. S

IRIU

NAS

Paoe

Num

ber

:1-B

To

tal P

age*

:l

Certi

ficat

e Da

te: 29

-JUL

-03

Invo

ice N

o. : 1

9317

648

P.O.

Num

ber

: Ac

coun

t :IE

B

SUffL

K

1943

01

1943

03

1943

01

1943

04

1943

0S

1943

0629

430*

19

4308

19

4309

1943

1019

4311

- 19

4313

19

4313

1943

14

2943

15

PRIP

CO

DE

308

308

308

308

208

208

208

208

208

208

208

208

208

208

206

226

336

336

336

336

326

336

326

336

336

336

336

326

336

336

Mo

Ut

Hi

P Pb

flb

ppi

\ pp

i pp

i pp

i pp

i

41

0.

06

13

370

0.11

13

38

00.

06

B 37

0 0.

06

11

360

0.11

7

310

0.03

18

IS

O 0.

03

17

330

0.01

6

80

0.03

34

19

0 0.

01

11

140

0.10

IS

3S

O 4

0.07

24

35

0 0.

1S

16

340

0.03

84

4

10

36

4 4

0.03

19

IS

O 6

4

CERT

IFIC

ATE

OF A

NALY

SIS

A931

7646

So

ST

Ti

Tl

0 V

ppi

ppi

* pp

i pp

i pp

i4

0.01

10

4

10

7 4

0.01

10

4

10

7 0.

01

10

4 10

4

4 0.

01

10

4 10

4

4 0.

01

10

4 10

3

0.01

10

10

19

0.

01

10

10

33

184

0.01

10

10

8

31

0.01

10

10

38

36

0.

01

10

10

134

S 0.

01

10

10

8 4

0.01

10

10

16

1

0.01

10

10

IS

1

4 0.

01

4 10

10

33

as 4

o.oi

4 10

10 17

N En

PPI

PPB

10

6 10

3

10

43

10

3 10

3

10

14

10

1410

10

10

30

10

14

10

6 10

13

10

8

10

130

10

13

CER

TIFI

CA

TIO

N:

Chem

ex L

abs

Ltd.

Analy

tical

Chtm

toti*

Oao

cham

Mi'

RagM

erad

Aiu

yere

6175

Tlm

bariM

Blvd

., M

laslss

auga

, On

tario

. Can

ada

UW

283

PHON

E: 4

16-6

24-2

806

o: N

R&

J RE

SOUR

CE A

SSOC

IATE

S LI

MIT

ED26

03 H

OLLI

NOTO

N OR

ES.

MI8

SISS

AUG

AON

L6K1

E8

Com

men

te:

AnN

: J. 6

IRIU

NA8

A831

9576

CERT

IFIC

ATE

A031

9576

N R

4 J

RESO

URCE

ASS

OCIA

TES

LIM

ITED

Proje

ct:

JENT

INA

P.O

.*:

aufc

adtte

d to

our

lab

in

Mia

aiea

awa,

OH

. T

his

repo

rt v

aa p

rint

ed e

a 29

-MM

-93.

SAM

PLE

PREP

ARAT

ION

W24

4

m 3

DESC

RIPT

ION

Ful

pi p

rer.

pre

pare

d at

Ctia

neii

ANAL

YTIC

AL P

ROCE

DURE

S

CHEM

EX

CODE 10

8610

57

1059

1060

1061

NUMB

ER

SAMP

LES

DESC

RIPT

ION

METH

ODDE

TECT

ION

LIMIT

UPPE

R LIM

IT

Cu *

i ru

eioa

- x

cr-J

tu

•i *

i ru

Biea

- Z

CV-JU

U Co

Hi

fliM

iea

- xc

v-ua

n

*i

Leoo

iad

uetio

n fu

raae

e re

\t

rusi

ea -

XCV

-US

Aa *

i ru

aioB

- X

CV-A

Ea

- xc

v-Au

- IC

9-U

* ru

iien

- IC

T-JU

M UC

O-XR

mra

cmi

raai

ea -

xcv

-Aia

fu

alea

- x

cr-

o.oa

0.09

0.01 0.02

0.1

0.01

20.0

20.0

10.00

40.0

100.0

10.00

Chem

ex L

abs

Ltd.

Analy

tical

Clwm

litt *

Qeo

chem

Wa * M

glstar

ed A

iuya

ra51

75 Tl

mber

tea B

lvd., M

lHlM

auga

, On

tario,

Can

ada

L4W

283

PHO

NE: 4

16-8

24-2

806

A N

R&

J R

ESO

URCE

ASS

OCI

ATES

UM

ITED

2803

HO

LLIN

QTO

N O

RES.

M

ISSI

S8AU

GA,

ON

L5K

1E8

Proj

ect:

JENT

INA

Comm

ents:

AT

TN: J

. 8IR

IUNA

8

TofaJ

Pag

es

:1 Ce

rtfflc

afe D

ate: 2

9-AU

Q-93

Inv

oice N

o. : 1

0310

676

P.O.

Num

ber

: Ac

coun

t :IE

B

CER

TIFI

CAT

E O

F AN

ALYS

IS

A931

9576

•AM

PLE

394303

394304

39

33

14

PB

EP

CODE

34

43

44

34

4

— —

—.

Cu *

1.2

C0

.88

18

.10

Hi <

0.

03

< 0

. 0

3-C

0.0

3

CO •C

0.0

1<

0.0

1K

0.0

1

8 *

(LO

CO

)

1.1

80

.78

18.3

0

F*

1.8

3.1

31

.9

Aa < 0

.01

< 0

.01

< 0

.01

CERT

IFIC

ATIO

N:.

Chem

ex L

abs

Ltd.

Analy

tical

crwm

toti *

Qao

oham

liti -

RagM

erad A

waya

ra61

76 Tl

mberi

es. B

lvd., M

lMiM

auga

, On

tario.

Can

ada

L4W

283

PHON

E: 41

6-62

4-28

06

j;

N R

ft J

RESO

URCE

ASS

OCI

ATES

LIM

ITED

2603

HO

LLIN

QTO

N O

RES.

MIS

SISS

AUQ

A.O

NL6

K1E

8

Comm

ents:

ATT

N: J.

SIR

IUNA

S

A931

9677

CERT

IFIC

ATE

A931

0577

N R

ft, J R

ESOU

RCE

ASSO

CIAT

ES L

IMIT

EDPr

otec

t JE

NTIN

A P.

OY#:

•aB

ploi

aub

Bitt

ad t

o ou

r la

b la

Mi*

aia

*hia

rep

ort

vaa

pria

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ea 3

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SAM

PLE

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ION

^P 20

5 22

6 22

*

NUMB

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it

DESC

RIPT

ION

Bann

han

riag

to

appr

o* 1

50 B

OBh

0-5

Ib o

ruab

and

api

i t

XCP

- AQ

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a ob

arg*

92 a

laav

aat

ICP

paok

ago

is a

uita

bla

for

trao

a aw

tala

la

M

il aa

d ro

ok •

••pi

***

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for

vhio

h tt

e ai

trio

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ogia

di

goit

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i* p

onib

ly i

nooa

vpla

ta a

roi

Al,

B*,

M,

ea,

Cr.

O*,

K, L

a, M

g, *a

, fer

, fi

, vi

, w

.

ANAL

YTIC

AL P

ROCE

DURE

S

CHEM

EX

CODE 10

0 2118

211*

2120

2121

2122

2123

2124

2125

2126

2127

2128

21

SO21

3021

312132

2131

2134

2135

213C

2137

2138

2138

2140

2141

2142

2143

2144

2145

2146

2147

2148

214*

NUMBER

[SAMPLES

DESCRIPTION

METH

ODDE

TECT

ION

LIMIT

UPPE

R LIM

IT

Aa ppb

i ruao 1

0 g

Ag PPB

I 32 o

loBoat, Mil

a rook

Al H

i 32 o

loBo

at, Mil

a rook rook

rook

rook

rook

rook

rook

rook

rook

rook

rook

rook

rook

•i Ca H

i 32

Cd p

pmi

32 o

lCo

PPB

I 32

ala

iMat

co

ilCr

PPB

I 32

ola

maa

t so

ilCu

PPB

I 32

ala

tMat

co

ilr*

Hi

32 o

lMM

at,

coil

al

32

OlM

MB

t B

Oil

i 32

olaMat

aoil

K Hi

32

ol

La PPB

I 32

Kg H

i 32 l

32

l 32 o

li•a H

i 32 o

li•i P

PBI

32

•oil a

rook

•oil

•oil

a

XC

P-A

UX

CP-

AU

X

CP-

AU

X

CP-

AU

X

CP-

AU

ICP-AM

XCV-AH

XCP-

zcp-

ICP-

rook

rook

rook

rook

rook rook

rook

ICP-AM

xcp-au

rook

rook

V PP

BI 32

olataaat,

Pb PPB

I 32 o

loBo

at,

rail

•b PPBI 32 OlOBWt, Mil

M PPBI

32 o

lOBoati. Mil

a ro

ok•r PPB

I 32 o

loBo

at, Mil a

rook

•i H

i 32

Tl P

PBI

32

O PPB

I 32 i

V PPBI

32 o

l W PPBI

32 i

la

ppB

i 32 o

:

XCP-AU

XCP-AM

XCP-AU

•oil a

•oil a

rook

, Boil a

rook

, Mil

a rook

, toil a

roo

k it,

Mil

a rook

XCP-AU

XCP-AU

XCP-AU

XCP-AU

XCP-AU

XCP-AU

XCP-AU

50.2

0.01 2 10 0. 0.01

0. 0.01 10 l

0.01 10

0.01 5 l

0.01 l 10 2 2 l l

0.01

10

10 l 10 2

10000

200

15.0

010

000

1000

010

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100.

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1000

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1000

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1000

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1000

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000

5.00

10000

1000

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000

1000

010

000

1000

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1000

010000

10000

1000

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Chem

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g

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Mg

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FA

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B pie

i pp

i na

*

ppm

ppa

ppa

ppa

% pp

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a %

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11

42

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abs

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Analy

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Cham

Ma *

Qaoc

hamM

a * R

aglat

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aaay

ara61

76 Tl

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lvd., M

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ada

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9577

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21 60.

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10

< 10

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3 630

<

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N;.

Chem

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Qeoc

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9578

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LIM

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Proje

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INA

P.O

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loa

auba

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d to

our

lab

in

Mia

aiaa

auga

, ON

. Vb

ia r

epor

t wa

a pr

inte

d on

24-

JUJO

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SAM

PLE

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ARAT

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w 205

226

238

em s 6 6

DESC

RIPTIO

N

Oaoo

baai

ring

to

appr

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50

0-5

Ib a

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and

apl

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abM

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gia

diga

atio

n

ANAL

YTIC

AL P

ROCE

DURE

S

CHEM

EX

CODE 10

0 6

NUMB

ER

SAMP

LES

DESC

RIPT

ION

METH

ODDE

TECT

ION

LIMIT

UPPE

R LIM

IT

Au p

pb:

ruao

10

g aa

avl*

n,

-AlB

5

1000

0 HH

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qua

ngi

a di

goat

JU

kB-BK

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om

0.2

100.

0

Chem

ex L

abs

Ltd,

Afwy

nnl C

hwnw

ti * u

Moh

wnl

itt51

75 Tl

mba

rlM B

lvd.. M

lMls

uuga

, On

tario.

Can

ada

UW

283

PHON

E: 4

16-6

24-2

806

To:

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A J R

ESOU

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ED28

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MISS

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ONL6

K1E8

Proj

ect:

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INA

Comm

ents:

AT

TN: J

. SIR

IUNA

S

l

Paga

Num

ber

:1 To

fil P

ages

:1

Cerft

icate

DatB

:24-

AUQ-

93

Invoic

e No.

: 103

1967

6 P.

O. N

umbe

r :

Acco

unt

:IEB

CERT

IFIC

ATE

OF A

NALY

SIS

8ANP

LB294217-

29

42

18

, 294219,

2942

20

2942

21

2942

22

PREP

CO

DE

209

209

209

209

209

209

226

226

226

226

226

226

Au p

pb

FA+A

A 50

80

<

5

75

Ag p

prn

Aqu

a R 4.2

8.2

0

.6

5.0

A931

9578

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S,0

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.

Chem

ex L

abs

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Analy

tical

Ctwm

Mi *

Qwxh

wnto

M' R

agMw

wt A

iuye

ra51

76 Tl

mbm

tea B

lvd.,

Mtoa

laaau

ga,

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io. C

anad

a L4

W 28

3 PH

ONE:

416

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6

j: N

Ra

J RE

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S LI

MITE

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MI8

SI88

AUQA

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L6K1

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Comm

ents:

ATT

N: J.

SIR

IUNA

S

A931

9570

CERT

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ATE

A931

9579

N R

A J

RESO

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ASS

OCIA

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LIMI

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ect

JENT

INA

P.O

.*:

taap

lai

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ad t

o aa

r la

b in

Mia

aiaa

auga

, *U

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port

MM

pri

nted

OB

91-M

Q-M

.

SAM

PLE

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ION

W

399

SAW

^K c

DESC

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ION

Pul

pi p

r*pp

*d o

n ot

bar

wor

feor

ter

ANAL

YTIC

AL P

ROCE

DURE

S

CHEM

EX

CODE 10

3*10

87

10B

(10B9

lOCO

1061

NUMB

ER

SAMP

LES

DESC

RIPT

ION

METH

ODDE

TECT

ION

LIMIT

UPPE

R LIM

IT

cu *

•i

*l

Flu

lOB

-

ZC

P-oe

li

ruel

oB -

m

*i

Looo

iad

oetio

B

ra i

n ra

eioa

- z

cv-

JU \

t ft

tele

a -

ICV-

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v-A

U

raal

on -

ZCP

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raai

oa -

o.oa

0.02

o.oi

o.o

a o.

i o.

oi

ao.o

ao.o

10.00

40.0

100.

010

.00

Chem

ex L

abs

Ltd,

Analy

tical

Cham

lata *

Qeo

ohem

lata *

Reg

latara

d Aaa

ayara

61

76 Tl

mbe

rfaa B

lvd., M

leat

oaug

a,

Ontar

io. C

anad

a L4

W28

3 PH

ONE:

416

-624

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6

r. N

R& J

RESO

URCE

ASS

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LIMI

TED

2803

HOL

LINQ

TON

CRES

. M

ISSI

88AU

GA, O

N L5

K1E8

Proj

ect:

JENT

INA

Comm

ents:

AT

TN: J

. SIR

IUNA

8

Page

N ar

:1

Total

Pag

es

:1 Ce

rtMca

fe Da

te:3

1-AU

Q-93

Inv

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o. : 1

8319

679

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Num

ber

: Ac

coun

t :IE

B

CERT

IFIC

ATE

OF A

NALY

SIS

A931

9579

SAM

PLE

2943

1729

4218

2942

10

2042

20

2942

21

2942

22

PU

PCO

DE

299

299

299

299

299

299

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CU

\

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CB

. SO

O

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0.0

6o.

oa4.6

4

Hi

* < 0.0

2

< 0

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< 0.0

2

4 0.0

2

t 0

. 02

< 0

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CO

H

< 0

. 01

< 0

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< 0.0

14

0.0

1

4 0.0

1

B t

(1*00)

2.8

9

0.4

60.4

7

0.0

6

0.0

3

4.6

8

r*

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7 1

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Chem

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Analy

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Chem

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Rag

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OH.

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SAM

PLE

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ION

w 944

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DESC

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ION

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; p

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pre

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mr

ANAL

YTIC

AL P

ROCE

DURE

S

CHEM

EX

CODE 97

5•7

7•7

6

NUMB

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MPLES

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THOD

DETE

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N LIM

ITUP

PER

LIMIT

Au p

pbi

XCV-

fluor

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*M*

p*ek

ag*

VA-X

CP-A

Tfl

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pbi

lCP-

fluoM

saav

e* p

aalu

o*

n-l

Cf-

Ut

ft p

pbi

XC

P-rl

uor*

ae*a

o* p

noka

o*

PA-IC

P-AT

010000

10000

10000

Chem

ex L

abs

Ltd,

Analy

tical

Cham

lata'

Qaoc

haml

ata *

Ragla

tarad

Aata

yera

5176

Tlm

berte

a Blvd

., Ml

eslea

auga

, On

tario.

Can

ada

UW

2S3

PHON

E: 4

16-6

24-2

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f. N

R 4

J RE

SOUR

CE A

SSOC

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S LI

MIT

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OLLI

NQTO

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mm

ents

: AT

TN: J

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SIUN

AS

il m

: 1

Toial

Pay

ee

:1 Ce

rtific

ate

Date

: 14-

SEP-

93

Invo

ice N

o.

: 193

2067

5 P.

O. N

umbe

r :

Acco

unt

:IEB

CERTIFICATE OF ANALYSIS

A9320675

SAMPLE

294203

294214

294217

294210

294222

PRIP

COBB

244

244

244

244

244

-~

Au ppb

ATS

23

112

74

10O

12 O

Pd ppb

ATS

< 2 4

< 2

< 2 2

Pt ppb

ATS

< a

< 10

< B

< B

X B

CERT

IFIC

ATIO

N:.

05/10/94 09:35 0705 360 1532 ROYAL OAK EXPL. QI002/002

ROYAL OAK AHALYTICAL LABORATORY CEEtTZETCATE OF ANALYSIS

DATE:

8

9"l

1112

13

14

15

16

17

18

19

20

21

22

24

LablB Chief CheB

07/04/94 09:32 O705 360 1532

ASSAI LABORATORIES 29-jm-94 BEPOEI

ROYAL OAK EIPL. 8002/002

HEP. 18686 PA6ESir j.

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0 0X212151

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BXR12161OZR12162 DXK12163OXR12164A

D DXR12151

BE FPH ICP0.6•—

<.S1.6 <.5 <.6 2.2 <.S

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110 285 126 678 683 121

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0.1 — - .

1.4 8.9 .6

3.9.6

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TA XICP

0.01" -^— .

2.81 .10 .84

1.46 2.80 2.74

FE XICP

0.01— —— — -Mm

1.37 9.661.29 2.96 4.28 1.38

CD PFHICP 1

'-" t -m m

<l •CI<l 11 ^

H.XICP

0.01•" ••MM—.

.43 1.62 .22 .66

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CO PPH ICP 1

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16 36 18 3415 16

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3.63 1.97 1.17 1.96 7.62 3.70

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65 6848 8937 57

SB PPH ICP 5

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7 ^6^ ^^

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666065800 5880

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15.3 86.2 60.6 90.8 86.3 15.6

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13 13 20 43 O 13

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2.7 3.8 .9

2.1 13.62 B• O

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13.6 2.8 9.1

16.8 712 13.2

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6961 4340

13667

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97.9 48.6 20.5 39.4

225 98.0

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590 634 699 768 76

630

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6 1 7 4

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Mining Actl on ttria tom to obMnad under ths authority ol MN MMno Act. This information wal to uMd lw correapondanca. Questions about

Ms cosodlon should lw dtaected to ine PiovkwW MsnsQsr, MWny Lands, IMnMiy of Northern Development end Mnss, Fourth Floor, 158 Coder Sheet, Sudbury. Ontario. P3E 6A5. tatsphons (70S) 870-7264.

Ontario

DOCUMENT No. 1 W94GO . c?UO W* '

B^M^^B^BB^^C^e^e^BM s9l^h^k^k^ O*M*^ ft r M^la^a) A 0*^1 AaeeMBAaB} aav 4^a Mtttfa^fte^K•lauucuona; - fioaso type or print ana suomn in oupucaie.- Refer to the Mining Act and Regulations for requlr

2.1570 8A separate copy of this form must be completed fi Technical reports and maps must accompany this A sketch, showing the claims the work is assignee

41J10SWOO19 2.1570B ALBANEL 900OHM NO.

JS*S3A 3/3

M or Q Plan6.1-30*

Frame To:

Woffc Performed (Check One Work Group Only)Work Group Type

Geotechnical Survey

Physical tndudtog DrMng

Other AutriortzedHf nHrnut K

Assays NOV 1 7 1994

MINING LAMPS l

Total Assessment Work Claimed on the Attached Statement of Costs S *J7sNote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Person* and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

flf.A.Us/LL

flan • fJnlal k*A^tau*iA* * g*.—— •x*—A — *ta — 4 **m*. ——— — - —*-*^DonvnciM 1111010*1 000 NOi0 ivo. i on I0v0f00 0100that at the iperfo i nw cWflw oovwsd In this woffc

in the currant hoktar'e name or held under a banalcWby the currant i

1 oertHy Hist 1 taw s psraonsJ knowtodgs of ttw twts sst forth In this Work Ms completion and amend report is trua.

t. having performed toe work or sama during andtor after

and of PHWM Cardfyfeig

&T O LASJData

For Offlc* Un Only

MwDeemed J

NoBca tor Amertdmenu Sam

AppiDMd X

Ml

RECEIVED-8 1994

aMifoaai)

Total Number ifl/O Total Value Work Total Value j Total Assigned Total Henry*

otCWms lvy Done J Work Applied v From \S

nut muxi *

*

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Credits you are daiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:

1. G Credits are to be cut back starting with the claim listed last, working backwards.

2. 69 Credits are to be cut back equally over all claims contained in this report of work.

3. G Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented.

MnA^ 1 - PWAIVM*!** Aff h^nafirlal liitar^at AIM iinrar rtntmtt trmnmtmtm fhj*il*kn aur^Min^ifciM •••••••m J —* - ~" -"* -— ** **A~ .~l*k m m m— m m*

to the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following:

l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature Date

Ontano

Ministry ofNorthern Development

Mines

Ministers du Devetoppement du Nord et des mines

Statement of Costs for Assessment Creditfetat des couts aux fins du credit d'evaluation

Mining Act/Loi sur les mines

Trans* cti

2.15?0 8Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining daim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands. Ministry of Northern Development and Mines. 4th Floor. 159 Cedar Street. Sudbury. Ontario P3E 6A5. telephone (70S) 670-7264.

Les renseignements personnels contenus dans la presente formute son! recueillis en vertu de la Lol sur le* mines et sen/iron! a tenir d jour un registre des concessions minieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers. ministers du Devetoppement du Nord et des Mines, 159. rue Cedar. 4* etage. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.

1. Direct Costs/Couts directs

Type

Wage* Satainn

Contractor'sand Consultant'sFaaaDroitsdel •fltrQpronMirat da ('expert-

SwppHMUMdFoumituresutilto*es

Equipment Rental Location de material

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Type

Type

t/

Amount Montan!

Totals Total global

Total Direct Costs Total des couts directs

2. Indirect Costs/Gouts indirects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work.Pour le remboursement des travaux de rehabilitation, tes couts indirects ne sont pas admissibtes en tant que travaux d'evaluation.

Type

Transportation Transport

1

Food and Lodging Nourrtture et hebergementMobilization and Demobilization Mobilisation et demobilisation

Description

Type

/T/L,/^

RE?Jb!VF.D

MOV 1 7 tt*

dlNIUG LAHtVSF-HANCH

L&&&SV&-

teoA

Amount Montant

/?7)5c

1 ————tif

1

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//S7^- 9t

IfV&.Q

73^Sub Total of Indirect Costs

Total partM des couts IndirectsAmount Allowable (not greater than 2OH of Direct Costs) Montant admissible (n'excedant pas 20 H das couts directs)Total VahM of Assessment CradM Valeur totato du crsdtt (ToM of Dlract and Allowable d'svakjattonIndhxLl fn*tm\ fToM do eadte draet*

Totals Total global

t

63760

'J 9(7 rf^ r

73S.U

Z&4

V7/M.S1•tin

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

: Le titulaire enregistr6 sera tenu de verifier tes depenses demandees dans le present etat des coots dans tes 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout on une partie des travaux d'evaluation presentes.

Filing Discounts Remises pour depot

1 . Work filed within two years of completion is claimed at 1 GtWb of the above Total Value of Assessment Credit.

1 . Les travaux deposes dans tes deux ans suivant teur achievement sont rer^*xxJrsesa1(X^%dela^raleortotalesusmemk>1^^ducrftcltd'^valuation.

2. Work filed three, four or five years after completion is claimed at 50*H) of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimed

x 0.50

2. Les travaux deposes trois, quatre ou cinq ans apres teur achevement sont rembourses a 50 "to de la valeur totate du credit d'evaluation susmentJonne. Voir les calculs ct-dessous.

Valeur tattle du credit d'evaluation

x 0.50

Evaluation totale demandee

Certification Verifying Statement of Costs Attestation de I'etat des couts

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as A? ASl(Recorded Holder. Agent. Position in Company)

to make this certification

J'atteste par la presente :que les montants indiques sont le plus exact possible et quo ces depenses ont ete engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formute de rapport de travail ci-joint.

l am authorized Et qu'a litre de je suis autorise(titulaire enregtstre. representant. poste occupe dans la compagnie)

a faire cette attestation.

Ministry of * Northern Development and Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

No. W9450 . o 00*7

Personal information collected on this torm is obtained under the authority of the Mining Act. This intormaten will be used for correspondence. Chiestions about this collection should be directed to the Provincial Manager. Mining Lands. Ministry of Northern Development and Mines. Fourth Floor. 159 Cedar Street. Sudbury. Ontario. P3E 6A5. telephone (705) 670-7264. ^. ^ ^2* 1570 8Instructions: - Please type or print and submit in duplicate. •w ~

- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining Recorder.

- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, snowing the claims the work is assigned to, must accompany this form.

ded HoUer(s) Cttont No.iffmsTT. stjkAu&y fi 3 A 3X59

Mining Division ^Township/Area

A-LAAM or Q No.

Z S? 3 To:Work Perfonned (Check One Work Group Only)

WorkGroup

IX

Geotechnical Survey

..Physical Work. Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

TJtefi/sM/fisS, SA-sn/HsA/t. AsAs2rov~r77*s^f

RECEIVPD

NOV1 1 : r54v

MINING LAN-..- t.HANCH

——— —— - ——————————

REnnRDED

— NOV - 8 1Q94 —

Receipt———————— - ———— -

Total Assessment Work Claimed on the Attached Statement of Costs S 2 J. 0*0. OONote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Perfonned the Work (Give Name and Address of Author of Report)

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sidel certify that at the time the work was performed, the claims covered in this work report ware recorded in the current holder's name or held under a beneficial interest by the current recorded holder. ft

Certification of Work Reportl certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report is true.

Name and Address of Person Certifying

. Lu/L X p V /Z. Se f/SfiA/S. JTelepone Date Certified By (Signature)

For Ofttee Use OnlyTotal Value Cr. Recordedli i frQ

j

Date Recorded

Doomed Approval Date ,

PI k 7/94

Mining Recorder . S

{-P ~L^1 ' f^^^L^ff'f)Date Approved /f

Date Nobce for Amendments Sent

Racaiv#su I!?rE. MARIE MIMNG DMSIOrY RECEIVED

^ NOV - 6 1994 pw

7.8.9.10,1X12,1,2.3.4.5.6

(841 (03*1) plN^ A

s*ifl\ C/j

^

,.

t i

SV.Ukl

"^. x^

^(K

**

•S

"S

^N•x.

-

^

vi

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-

^

5Kl

^

||ffl

" 3

-^oii!|

SiJS3 |

iiri

Is1li

00k0

*F*^s

fs• r

i

Mil

RFC

NOV

ING '.

E---J

.71:

;NDSI

r D)34

r ..iic

•-—:

1

j

'

ifeQ

•si

S6

iQ^

*s^^5O

^4

rx

x^•^

s0

^N

V

^0

^

N^^

,M^\

?0

ilflf*s~

lift

ff

i *

Xf^\ H

^

l *t1

0

tNLCc

^x

cQcs

^*x

5

b

gt(o{rf m ffltp l\ c

Kl

^g0

CV

^1

S

V

5 >oio e.P*-

n*7* ^

Credits you are daiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:1. D Credits are to be cut back starting with the claim listed last, working backwards.2. j*3 Credits are to be cut back equally over all claims contained in this report of work.3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented.

UA*A 1 - FwmmrklA* nf KArkAffl^l*! intiir^at Arm unrar nrrlari innmimrm rtntlAn A*inAAm*nt* •••••••lil mnhim f\f wir*Ann*nta Atf* with rmtrMT't

to the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following:

l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature Date

Ontario

Ministry ofNorthern Developmentand Mines

M. ,t6re du Devetoppement du Nord et des mines

Statement of Costs for Assessment CreditEtat des couts aux fins du credit devaluation

Mining Act/Loi sur les mines2.1570 S

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining daim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands. Ministry of Northern Development and Mines. 4th Floor. 159 Cedar Street. Sudbury. Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presents formula sont recueillis en vertu de la Lot sur les mines et serviront a tenir a jour un registre des concessions minieres. Adresser touts question sur la collece de ces renseignements au chef provincial des terrains miniers. ministers du Devetoppement du Nord et des Mines. 159. rue Cedar, 4e etage. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.

1. Direct Costs/Couts directs

Type

—.

Satalras

Contractor's and Consultant's FeesDraitsde ('entrepreneur et de ('expert-

Supplies Used Foumitures

Equipment Rents! Location de materiel

Description

Labour Main-d'oeuvreReid Supervision Supervision sur to terrain

Type

y&dx TffrType

Type

Amount Montan!

7/7 W

Total Direct Costs Total des couts directs

Totals Total global

252*2.

2. Indirect Costs/Couts indirects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work.Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admissibles en tant que travaux d'evaluation.

Type

Transportation Transport.^.

4 \"f '-~- i ~j ^ : '.. -, f C

| NCV 1 '

1 KlKjlN-j uAt,

Food and Lodging Nourrtture et hebergementMobilization and Demobilization Mobilisation et demobilisation

Description

Type

~fL3fl' \ ' f r* - ''"•'•'.i..1- ;

i

,.-,. ji j J T ,

pS t -UNC.'i ( ———————

L&bf/vt' f**J*

Amount Montan!

**867Z

1,721-K

6?o.Tp

i?1.fASub Total of Indirect Coats

Total partM des couts indirectsAmount Allowable (not greater than 20* of Direct Coats) Montant admissMe (n'excedant psi 20 H des coots directs)Total Value of Assessment Credit Vatour totato du credK (Total d Direct and Afcwabto d'tvahiadon IndkBd ctMtet rToW dm cotti dtaeh

Totals Total global

1

s*e.7j

?.U1Z*

U9./6

7.014JV* ~

22 0*0.

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 jours suivant une demands a cet effet. Si la verification n'est pas effectuee. le ministre peut rejeter tout ou une partie des travaux d'evaluation presentes.

Filing Discounts Remises pour depot

1. Work filed within two years of completion is claimed at 100*ft of the above Total Value of Assessment Credit.

Les travaux deposes dans les deux ans suivant tour achevement sont remb(Xlrsesa100%ctelavaleurtotatesusn1e^tx>^nee(luCTftdHd'&valuatlon.

2. Work filed three, four or five years after completion is claimed at 5Cm of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50

2. Les travaux deposes trois, quatre ou cinq ans apres tour achevement sont rembourses a 50 M de la vatour totato du credit d'evaluation susmentionne. Voir tos caJculs ct-dessous.

Vateur totato du credit devaluationx 0,50

Evaluation totale demandee

Certification Verifying Statement of Costs Attestation de I'etat des couts

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as(Recorded Holder. Agent. Position in Company)

to make this certification

J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont ete engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formuto de rapport de travail ci-joint.

l am authorized Et qu'a litre de je suis autoris6(titulaire enregistre. representant. paste occupe dans la compagnie)

a faire eerie attestation.

Signature Date

0212 (OU91) Nota : Dans cette formule, kxsqu'il designe des personnes. le masculin est utilise au sens neutre.

OntarioMinistry ofNorthern Developmentand Mines

Minister® duOeveloppement du Nord et des Mines

Geoscience Approvals Office 933 Ramsay Lake Road 6th Floor Sudbury, Ontario P3E 6B5

February 22, 1995

Telephone: (705) 670-5853 Fax: (705) 670-5863

Our File: 2.15708 Transaction /: W9450. 00086

W9450. 00087

Mining RecorderMinistry of Northern Development 6 Mines60 Church StreetSault Ste. Marie, OntarioP6A 3H3

Dear Madam Kurylo:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS 1197219 et al. IN ALBANEL 6 NICHOLAS TOWNSHIPS

All deficiencies associated with this submission have been corrected. Accordingly, assessment work credits have been approved as outlined on the attached distribution of work credit form. The credits have been approved under Section 9 (Prospecting), Section 10 (Physical), Section 12 (Geology) and Secton 17 (Assays) of the Mining Act Regulations.

The approval date is February 20, 1995.

If you have any questions regarding this correspondence, please contact Steven Beneteau at (705) 670-5858.

ORIGINAL SIGNED BY:

Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

SBB/jl Enclosure:

cc: Resident GeologistSault Ste. Marie, Ontario

Assessment Files Library Sudbury, Ontario

REPORT OF WORK FORM

Please note, the assessment credit has been distributed to reflect the value of work performed on each claim.

FEBRUARY 22, 1995 FILE: 2.15708 TRANSACTION f W9450.00087

VALUE OF ASSESSMENT CLAIM WORK DONE

1197221 $ 863.001197220 $ 863.001197219 ^ 863.001118612 $19,888.001118613 $ 6,400.00

TOTAL $28 / 877.00

FILE: 2.15708 TRANSACTION i W9450.00086

VALUE OF ASSESSMENTCLAIM WORK DONE

1186888* $10,042.001186887* S 550.001186886* S 1,218.001118694' $ 1,060.001118693. ^ 1,881.001118695* S 3,377.001118696* $26,345.001118697 S 0.00 NO ASSESSMENT WORK PERFORMED1186889 $ 0.00 NO ASSESSMENT WORK PERFORMED

TOTAL $44 / 473.00

l/D

O

LU

fm

Ol lCD

MWatry ofNaturalResources

Mnistry ofNorthern Developmentand Mines

Ontario

DOCUMENT No. VY9450

INDEX TO LAND DISPOSITION

PUN

G-3257TOWNSHIP

ALBANEL

M.N.R. ADMINISTRATIVE DISTRICT

BLIND RIVERMINING DIVISION

SAULT STE. MARIELAND TITUS/REGISTRY DMSIOM

ALGOMA

.1570

RECEIVED

NOV l 71994

MINING LANDS BRANCH

1:2* M*

1*1

Contour littoral 10 Motrao

AREAS WITHDRAWN FROM DISPOSITION

SYMBOLS

i- Mining Rights Only WO* Surface ftghta Only H * S - Mining and Surface Rights

BoundaryTownship. Maridlan, Baseline.

Road allowance; surveyed . . . .shoreline . . .

Lot/Concession; surveyed... unsurveyed

Pare**; surveyedunaurveyad . . ... . ...

Hight-e*-way; road . . . .

KSEHVED FQfl PUBLIC USE

utWty.

Reservation. emr, p*t, ma...Contour .. ,. . ..

Interpolated . Approximate Depression. .

SfC.M/eO Vf.fi/St IS/lt/M I.R.O. 9.14*4

Control point (horizontal) ..,................................... A

Flooded land....................................., r-i-i-r—i-i-i-i-i-r

Mine head frame .............................................. a

Pipeline (above ground) ............................ ——— ———

Railway; single track..............,........,....... ———-———double track.............................. -*——M——*-abandoned.......................,....... -*— —— —*-

Road: highway, county, township .................... ^^———--™access ...................................,. ^——™™—~trail, bush................................... ————————

•Shoreline (original).................................

Transmission lin*.................................. —-———-—

WbodadanM.....................................

(j*

DISPOSmON OF CROWN LANDSPatent

Surface A Mining Rights Surface Rights Only Mining Rights Only

LeaseSurface 4 Mining Rights Surface Rights Only Mining Rights Orrty

Licence of Occupation ........................................ .T

Ordar-in-Counctl............................................. .OC

RIGHTS *W SSH 189513,416366 (SEE ONTAWO

QAETTE-MAY 9/92

FACE B MHNe RK3HTS SSM 389624,416366.416367

FOR PBOSPECT1IW.3TAKING QUT.SALE AT 7-OO AM STANDARD TWE JUNE 1/92.

S RUT OFCLAM SSM SBCXTOW WraSPECTINft ST1UWG OUT. MLC OR LEfiflt

7-00 Ml STANDARD THE JUNE 1*4

ONTARK) fiAZETTE WAY 14/94*) THAT MAP lLED

RCES

B a

Canceled

THE INFORMAAPPEARS ONHAS BEEN CFROM VARIOUSAND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKE MlN- ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.

Sand 4 Gravel .

^F^^^^tf^*^^^^^?

Th* 195O" Chang*

A, ta,

MiM*

Map base and land disposition drafting by Surveys and Mapping Branch. Ministry of Natural Resources.

The disposition of land, location of tot fabric and parcel boundanes-on

41J10SW0019 2.15708 ALBANEL 200

\

^WB^ww^W

Ministry ot Ministry ofNatural Northern DevelopmentResources and Mines

Ontario RECEIVED

FEB 2 INDEX TO LAND DISPOSITION

G-3257TOWNSHIP

ALBANEL

M.N.R. ADMINISTRATIVE DISTRICT

BLIND RIVERMINING DIVISION

SAULT STE. MARIELAND TITLES/REGISTRY DIVISJ2N

ALGOMA

Scale 1:20 MM

t 11

IMS t II MM 500* 1*1

Contour Interval 10 Metres

SAULT STE DATE OF ISSUE

FEB 24 1995

SAULT STE. MARIE MINING RECORDER'S OFFICE

'i:

(AREAS WITHDRAWN FROM DISPOSITION

MRO- Mining Rights OrtfySRO- Surface Rights On*yM +1-Mining and Surface Rights

SYMBOLS CMvN*. FS*

BoundaryTownship, Meridian, Baseline.

Road allowance; surveyed... .shoreline...

Lot/Concession; surveyed... unsurveyed

Parcel; surveyedunsurveyed .........

Rtght-c* way; roedrariway ........utHtty... ...

Reservation ........ L.......

Cliff, Prt, Prte . ... .

ContourInterpolatedApproximate

Depression.................

Qj) HESEHVEO fQH PUBLIC USE U3SS6

V S EC.36/SO W.6/A2 IS/H/CK S.ft.O- *I494

(VT) tffVSfo ^/v^f f a/f,

Control point (horizontal) ...................................... A

Hooded land....................................., z-l-l-l-l-l-l-l-l-l-l

Mine head frame .............................................. a

Pipeline (above ground) ............................ ——— ———

Railway; single track...,...,....................... ———-——•~double track.............................. --——-———abandoned............................... -*— —'— —l-

Road; highway, county, township .................... =e ==access ..................................... =====—=-trail, bush................................... ——————

Shoreline (original).................................

Transmission line.................................. —*———-——

VttxxJed area......................................

-**

J 5AA-

DISPOSITION OF CROWN LANDSPatent

Surface A Mining Rights Surface Rights Only Mining Rights Only

LeaseSurface 4 Mining Rights Surface Rights Only Mining Rights Onty

Licence of Occupation ........................................ .T

Order-in-Councd............................................. .OC

Cancelled . ..................................................9

l MINING RIGHTS O*y SSM 389513,41*368 (SEE ONTARIO

GAETTE-MAY 9/9?

SURFACE a MINING RIGHTS SSM 389624.4i6366.ti6367OPEN FOH PROSPECTING.STAKiNG OUT,SALE AT 7-00 AMSTANDARD TIME JUNE 1/92.

1.0-1*5 PART OfCUUM SSM 8322OPEN FOR PROSPECTING. STAMNG OUT, SALE Ofl LEASE AT 7-00 AM STANDARD TIME JUK 1/S4

(SEE ONTAWO GAZETTE MAY w/M")

.e

.Q

B .B

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ' ON THE STATUS OF THE LANDS SHOWN H6REON.

Reservation.. -

Sand A Grave*.

The l Appr ox, -

Haanelic Be*ring* w7 Annrj *- ' r ^ *- fl

Map base and land disposition drafting by Surveys and Mapping Branch. Ministry of Natural Resources.

The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only.

s

. l*LO

41J10SW0019 2 .15708 ALBANEL 210

"~ U(S

tt l ift HIl . *V- l l

^ t -j*T . v, -1/ ;*.m Cu. 9.M B* A**/T ^

* ~— J^*(U* *V** I*.*' - BMCw *var li,*' - CM

-J ^X i

DH

CH

GR

—— #

* B rv

GKOLOGT LEGEHD

middle precanbrian

VIpiseIng Diabase, Gabbro

HUROHIAI SUPERGROUP

ELLtOT LAKE GROUP

Dollyberry Lake Format ion- andeslte/basalt

COBALT GROUP

Bar River Foraa11on- orthoquartzite

Gordon Lake Formation- sandstone and siltstone

Lorraln Format i on- sandstone and conglomerate

Gowganda Formation- naInly conglomerate, arkose, feldspathic

sandstone and siltstone

QUIRKE LAKE GROUP

Serpent Format Ion- feldspathic sandstone, arkose, calcareous

sandstone, minor siltstone, conglomerate

Espanola Formation- limestone, dolomite, calcareou; calcareous sandstone, sil tston

Bruce Farmatlon- polymictic conglomerate, greywa

HOUGH LAKE GROUP

Klsslssagl Formation- feldspathic sandstone

archaen

Granitic Intrusive Rocks- monzonite, granodiorite, trondhjemite

Gneissic Intrusive and Mlgmatltlc Rocks- ortbognelss, migmatite, amphibolite

Ketavolcanic and Hetasedlmentary Rocks- mafic-feIsle volcanics, minor sediments

SrHBOLS

regional faults

local faults and airphoto lineaments

base-precious metals (mainly copper)- bearlng structures (shear zones, quartz-chlorlte t/- albite breccia zones and/or quartz-carbonate ve l ne)

. copper occurrence

. drill hole

. chip channel sample

. grab sample

PREVIOUS WORKERS

Albanel Township

Plcton Uranium Mines Ltd., 1955-68

Canamlska Copper Mines Limited, 1965—66

Hanna Mining Company, 1969

Stanford Mines Limited, 1971-72

Fort Warman Explorations Inc., 1974-75

United Reef Petroleums Limited, 1986

Micholae Township

Gowganda Silver Mines Limited, 1972

for

i.J. Roy- 4 ~

AREA GEOLOOY, STRUCTURES and MINERAL OCCURRENCES

IB&J RBSOURCH ASSCTIATBS LIIITED

Kap lo.: la. Albanel Twp.Compiled bv: I.Prawn by: I.

Willoughby Willoughby

Date: 31 August. 1994Scale: 1:20.000

Sources: Siemiatkowska, 1978; Anthony and Vllloughby, 1936.AB6es6Bent Piles, HDM, Sault Ste. larle ae at 19O4, Vtlloughby (mapping reGults, this project), 1994.

41J10SW0019 2.15708 ALBANEL 220

"W \ *

j.-'

13

DH

CH

GR

GEOLOGY LKGEMD

•Iddle precambrian

nipissing Diabase, Gabbro

HUROBIAI SUPERGROUP

ELLIOT LAKE GROOF

Dollyberry Lake Farnatian- andeslte/basalt

COBALT GROUP

Bar River Formation- orthoquartzite

Gordon Lake Formation- sandstone and siltetone

Lorraln Forma 11on- sandBtone and conglomerate

Gowganda Formation- mainly conglomerate, arkose, feldspathic

sandstone and siltstone

QUIRKE LAKE GROUP

Serpent Formation- feldspathic sandstone, arkose, calcareous

sandstone, nlnor siltstone, conglomerate

Espanola Formation- 11 meetone, dolomite, calcareous-non-

calcareous sandstone, siltstone

Bruce Formation- poiynlctlc conglomerate, greywacke

HOUGH LAKE GROUP

Vlsslesagl Formation- feldspathic sandntone

archaen

Granitic Intrusive Rocks- monzonite, granodiorite, trondhjemite

Gneissic Intrusive and Xigmatitlc Rocks- orthngnelss, migmatite, amphibolite

Metavolcanlc and Hetasedlnentary Rocks- maflc-felslc volcanics, minor sediments

SYMBOLS

regional faulte

local faulte and airphoto llneanente

base-precious raetale (maInly copper)- bearlng structures (shear zone**, quartz-chlorite -t/— albite breccia zones and/or quartz-carbonate veins)

. copper occurrence

. drill hole

. chip channel sample

. grab sample

1570PREVIOUS WORKERS

Albanel TownshIp

... Plcton Uranium Mines Ltd., 1955-68

. . . Canamiska Copper JClnes Limited, 1965-66

... Hanna Mining Company, 1969

... Stanford Mines Limited, 1971-72

... Fort Herman Explorations Inc., 1974-75

... United Reef Petroleums Limited, 1988

Ylcholas Township

... Gowganda Silver Mines

MineMINING

for

A. J. Roy

AREA GEOLOGY , STRUCTURES anti MI NERAL OCCURRENCES

RESOURCE ASSOCIATES LIICITHD

Map In. ; l b. Ilchdlas Twp.Co api led by: 1. VlUoughby Drawn by: I. WilloughbyDate: 31 August. 1994Scale: 1:20.000

Sources: Siemiatkowska, 1978; Anthony and Vllloughby, 1988,i6BeeB*ent Piles, HDM, Sault Ste. Marie as at 1904,

Vllloughby (mapping results, this project), 1994.

41J10SW0019 2.15708 ALBANEL 230

DETAIL DRILL HOLE IIPOBMATIOI

Scale: l" - 20 ft. ; up dip projections to surface, assuming average 50 deg south dip of mineralized zone (however no bedding/structure information indicated from drill sections); copper values in l over sampled core interval shown.

tf-13

l**'

El anomaly axis

soil geochemical survey line, mull copper value indicated

drill hole location

Canaaiska property boundary (1965)

Jentina property (1994)

2. 1570 8

LtfNtlVG LANQSflfcfife/

P r-0.1 eo-fc

for

i.J. Boy

EXPLORATION DATA COMPILATION, CANAMISKA COPPER MINES LTD., l 965

JBSjQQKClB^AJiSOCIATES^IIITlD

Map

Of*m \

mno Abv: I. Vlllnimrhbv

I. Vt l lonvKbvPate: 31 Amrogt. 1994Scale:' l* * 300 ft. tfWSources: le-Interpreted from HDM (Sault Ste. Marie)

File AlbMMl 0031-4.knt

41J10SW0019 i 15708 ALBANEL

•** ^ •—- ^

H P -^ _ ^jr Z — — ^-_ s

FALG0NBRIDGE PATENT

O \ 0oz AuXT, 3 46 or Ag/TCut-Pb.Zn.Co, S. ( 1969)

PffltM-

, - -

MAP SYMBOLS

area of outcrop exposure

small outcrop

geological contact, defined, assumed

fault, indicated or interpreted from mapping andXor aerial photographs

approximate axial trace cf anticline or antiform

approximate axial trace of syncline or synform

strike and dip of bedding, tops indetermmed,tops determined, bedding overturned

strike and dip of schistosity, cleavage , inclined, vertical, 1st order

strike and dip of schistosity, cleavage ; 2nd order

small fold w plunge indicated, s-symmetry, z-symmetry

strike and dip of fracturing

strike and dip of quartz vein

strike and dip of shear zone

strike and dip of jointing, inclined, vertical

trench , small, large

pit , small, large

968 rock sample series w precious -base metal anomalous assay values

1994 rock sample series, assayed for Cu, Au, Ag

character sample

jn fi vets ZABBREVIATIONS

weakly-moderately alteredbreccia, brecciatedcarbonatized(area) forest clear cut harvesteh Ion 11 zedchalcopyritecarbonate vein letsgalenagraded bedding, rhythmic layering"hemaritizedmalachitemagnetitepyrrhotitepyritesilicifiedquartz stringersquartz vein

Sources. 1994 mapping program, OGS Map 2399, Endikai Lake, 1974

GEOLOGY LEGEND

921 j 91

936[ 8 l

901 l 7 l

923945912962

93G| 3 l

903-1 3 j

9481 2 l

910 j \ l

Mipissmg Diabase, Gabbro- undifferentiated

HURONIAN SUPERGROUP

COBALT GROUPBar River Formation

- light gray quartzite, massive-bedded, ripple marks

Gordon Lake Formation- buff-pink interbedded sandstone and siltstone

Lorrain Formation- hematitic pebbly sandstone, conglomerate

{not represented in 1994 survey area)

Gowganda Formation- d reddish arkosic sandstone-c red-pink granite and arkose pebble-cobble conglomerate-b grey-grey green siltstone,quartz-rich (quarzitic) siltstone-a grey heterolithic conglomerate

QUIRKE LAKE GROUP

Serpent Formation- pinkish to Tight grey-green feldspathic quartzite

Espanola Formation-b clastic sediments , mainly grey-grey green siltstone with

some quarzitic, calcareous siltstone X sandstone- a non-clastic sediments , mainly brown weathered limestone

with some dolomite and cherty horizons , generally laminated with thin siltstone laminations

Bruce Formation- greenish grey polymictic conglomerate, greywacke

HOUGH LAKE GROUP

Mississagj Formation- pink-green feldspathic sandstone, arkose

(MIMZRAUZED) BRECCIA/VEIN ZONES and associated ALTERATION

931'l C

918 l AQ

925 j BX

942 j AA

929[ QCV

909[TSS

956|SCS

chlorite alteration zone with some associated shearing

albite-silica alteration zone

quartz -chlorite -t- f- albite breccia zone with some Fe-carbonate

ci bite alteration zone

late quartz-carbonate veinmg, stringers and stockwork

talc-sencite (actinolite?) - chlorite schist X breccia zone

sericite - chlorite (*X-carbonate) schist

iVED

1995

Jentina Mine Projectfor

A.J. Roy

GEOLOGY AND MINERALIZED STRUCTURES

NR8J RESOURCE ASSOCIATES LIMITED

Mbp No. Map l , SW Sheet DateCompiled by N WilloughbyDKN*I by B Fa l (ado

31 August, 1994Scale

250\

tgofLf2f ^ __ ^

TRENCHES. DRILLING 1950*3

HW*

T - ^r~

li

SI

S2

TO

sz•o

O . CD

* 3935

* 9418

W9423

7- 7 -

MAP SYMBOLS

area of outcrop exposure

small outcrop

geo logical contact j defined, assumed

fault, indicated or interpreted from mopping and /or aerial photographs

approximate axial trace of anticline or antiform

approximate axial trace of syncline or synform

strike and dip of bedding , tops undetermined, tops determined, bedding overturned

strike and alp of schistosity, cleavage , inclined, vertical i 1st order*

strike and dip of schistosity, cleavage ; 2nd order

small fold m plunge indicated, s -symmetry, z- symmetry

strike and dip of fracturing

strike and dip of quartz vein

strike and dip of shear zone

strike and dip of jointing, inclined, vertical

trench, small, large

pit , small , large

1986 rock sample series w precious -base metal anomalous assay values

1994 rock sample series, assayed for Cu, Au, Ag

character sample

Sources -. 1994 mappi

ABBREVIATIONS

ALTE weakly -moderately alteredbx breccia, brecciatedcarb carbonatizedc c. (area) forest clear cut harvestchl chtonttzedcp chalcopyritecvt carbonate vein letsgn galenaGb graded bedding, rhythmic layeringhem nemo Wiredmal malachitemte magnetitepo pyrrhotitepy pyritesil silicifiedq str quartz stringersqv quartz vein

program; OGS Mop 2347, Nicholas a Raimbault Twos, 1969.

GEOLOGY

9 l

19361 6 j

l 7 l

l 1*1

923945912962

END

lawng Dta base, Gabbro-••differentiated

HUrVMNAN SUPERGROUP

COBALT GROUPBar flintr Formation

- ttgJ* gray quartzite, massive-bedded, ripple marks

Gordfa Late Formationr

-buff-pink interbedded sandstone and siltstoneLorram Formation

-fcMMhtte pebbly sandstone, conglomerate l not represented in 1994 survey area)i

Gowganda Formation- *l veddwli arkosic sandstone-t MeVpMfc granite and arkose pebble-cobble conglomerote-b. ami fjey green siltstone,quartz-rich (quarzitic) siltstone-la. fray Marotithic conglomerate

LAKE GROUP

1930131

3 l

l 9481 2 l

Ser

Esp

Brua*

(MINERALIZED)

to light grey-green feldspathic quartzite

itionsediments, mainly grey-grey green siltstone with

i tic, calcareous siltstone X sandstone sediments , mainly brown weathered limestone

dolomite and cherty horizons , generally laminated siltstone laminations

grey polymictic conglomerate, greywacke

LAKE GROUPFormation

feldspathic sandstone, arkose

CCrA/VEHt-ZONES and toted ALTERATION

918 l

l 925 1 BX j

|942| AA]

j 929| QCV]

l 909| TSSl

j 956 j SCS| seri

chloBp alteration zone with some associated shearing

otbi&Miico alteration zone

quorjpj^btorite -t- /- albite breccia zone with* some Fe-corbanotialbi^B^pleration zone

late'ei^rte-corbonate vening, stringers and stockwork

talcHMldte (actinoliteP) - chlorite schist7breccio zone

te U J- carbonate) schist

RECEIVED

FEB9 1995

Jtntina Mint Projectfor

A. J Roy

GEOLOGY AND MINERALIZED STRUCTURES

ISJ RESOURCE ASSOCIATES LIMITED

Map No. Date 31 August. 1994Compiled by WilloughbyDrawn by Fallodo

—ir2——.*l X S

NO. 2 COPPER-BE API N

RtGHFUXOVERTICALHOLE P2 (1967)ARCHEAN VOLCANICS (?)AT40OO

^*1"^l3h^i

n^ri

//WC*7**A^

-aft

—LU8

-4-)ut**bfrtf

MAP SYMBOLS

area of outcrop exposure

smaH outcrop

geological contact; defined, assumed

fault, indicated or interpreted from mapping and /or aerial photographs

approximate axial trace of anticline or antiform

approximate axial trace of syncline or synform

strike and dip of bedding} tops indeterminedt 1ops determined, bedding overturned

strike and dp of schistosity, cleavage ; inclined, vertical , 1st order

strike and dip of schistosity, cleavage; 2nd order

small fold w plunge indicated, s -symmetry, z-symmetry

strike and dip of fracturing

strike and dip of quartz vein

strike and dip of shear zone

strike and dip of jointing, inclined, vertical

trench , small , large

pit , small, large

(988 rock sample series w precious -base metal anomalous assay values

1994 rock sample series, assayed for Cu, Au, Ag

character sample

ABBREVIATIONS

ALTEbxcarbc c.chlcpcvtgnGbhemmalmtepopy silq str qv

weakly-moderately alteredbreccia, brecciatedcorbonotized(area) forest clear cut harvestdtloritizedchalcopyritecarbonate vein letsgalenagraded bedding, rhythmic layeringhematttizedmalachitemagnetitepyrrhotitepyritesilicifiedquartz stringersquartz vein

mapping program.

r*

ln

GEOLCfeY LEGEND

190' l 7|

modi

923945912962

l

1930 [ 3 |]

19031 3

Nipissing Diobose, Gabbro- undifferentiated

HURONIAN SUPERGROUP

COBALT GROUPBar River Formation

- light gray quartzite, massive-bedded, npple marks

Gordon Lake Formation-buff-pink interbedded sandstone and siltstone

Lorrain Formation- hematittc pebbly sandstone, conglomerate

{not represented in 1994 survey area)

Gowganda Formation- d. reddish arkosic sandstone-c red-pink granite an* arkose pebble-cobble conglomerate-b. grey-grey green siltstone,quartz-rich (quarzitic) siltstone-a grey heterolithic conglomerate

QUIRKE LAKE GROUPSerpent Formation

- pinkish to light grey-green feldspathic quartzite

Espanola Formation-ta. dashc sediments; mamly grey-grey green siltstone with

some quarzitic, calcareous siltstone/sandstone-a non-clastic sediments , mamly brown weathered limestone

with same dolomite and cherty horizons , generally laminated with thm siltstone laminations

Brace Formation~ greenish grey polymictic conglomerate, greywacke

HOUGH LAKE GROUPissagj Formation

- pin k-green feldspathic sandstone, arkose

(MINERALIZER BRECCIA/VEIN ZONES and associated ALTERATION

93l| c

9181 AQ

9251 BX

9421 AA

chlorite alteration zone with some associated shearingaibite-silica alteration zone

quartz-chlorite ^/-albite breccia zone with some Fe-carbonatealbite alteration zone

tale quartz-carbonate vein mg, stringers and stockwork

talc-sericite (actinolite P) - chlorite schist X breccia zonesericite-chlorite (* A carbonate) schist

RECEIVED

FEB9 1995

Jtntino Mine Projectfor

A.J. Roy

GBDLOGY AND MINERALIZED STRUCTURES

NR8J RESOURCE ASSOCIATES UMtTEO

IS)OB O

ClOUS METAL- STRUCTURE

Q.030% Cu 0015"^!*

TO

SO^A-5

S220

SZ

•O

e , cri

* 3935 ]

* 9418

W9423

MAP SYMBOLS

area of outcrop exposure

small outcrop

geological contact ; defined, assumed

fault, indicated or interpreted from mapping and /or aerial photographs

approximate axial trace of anticline or antiform

approximate axial trace of syncline or synform

strike and dip of bedding, tops tndetermined, tops determined, bedding overturned

stnke and dp of schistosity, cleavage , inctmed, vertical , l st order

strike and dip of schistosity, cleavage, 2nd order

small fold w plunge indicated, s -symmetry, z- symmetry

strike and dip of fracturing

strike and dtp of quartz vein

strike and dip of shear zone

strike and dip of jointing-, inclined, vertical

trench, small, large

ptt , small , large

1968 rock sample series w precious -base metal anomalous assay values

1994 rock sample series, assayed for Cu, Au, Ag

character sample

miABBREVIATIONS

ALTE weakly -moderately alteredbx brecaa, brecciatedcarb carbonatizedc c. (area) forest clear cut harvestchl chtontizedcp chalcopyritecvt carbonate vein letsgn galenaGb graded bedding, rhythmic layeringhem nemo fi ri zedmal malachitemte magnetitepo pyrrhotitePV pyntesil silicifiedq str quartz stringersqv quartz vein

~ 2?-jH

Sources. 1994 4appmg program; Anthony and Willoughby, 1986; OGS Map 2399, Endikoi Late, 1974.

GEOLOGY LEGEND

92' l 9 l

l 936 1 8 l

\ l

923945912962

Nip ssing OKI bo se, Gabbro- undifferentiated

HURONIAN SUPERGROUP

COBALT GROUP

Bar River Formation-light gray quartzite, massive-bedded, ri ppi e marks

Gordon Lake Formation- buff-pink interbedded sandstone and siltstone

Lorrain Formation-hematite pebbly sandstone, conglomerate

(not represented m 1994 survey area)i

Gowganda Formation-d. reddish arkosic sandstone-c red-pink granite and arkose pebble-cobble conglomerate-b. grey-grey green siltstone,quartz-rich (quarzittc) siltstone-a grey heterolithic conglomerate

J9031 3 l

|948| 2 l

QUIJRKE LAKE GROUP

Serpent Formation- pinkish to light grey-green feldspathic quartzite

Espewdo Formation-b. dexhc sediments, mainly grey-grey green siltstone with

! sane quorzitic, calcareous siltstone /sandstone^clastic sediments , mainly brown weathered limestone

\ dolomite and cherty horizons, generally laminatedsiltstone laminations

\ Brute Ruination

tsh grey polymictic conglomerate, greywacke

HOtfGN LAKE GROUP

Mi formationfeldspathic sandstone, arkose

(MINERALIZED) 3RECCIA/VEIN ZONES and associated ALTERATION

931 l

918 l AQ l tb|^t

925 j BX

942J AA l

9291 QCVl

alteration zone with some associated shearing

albfte-silica alteration zone

qua|t*-cMDnte-*- /-otote brecaa zone wtth some Fe- carbonate

alb** alteration zone

late| ajuartz- carbonate vein mg, stnngers and stockwork

909|TSSl talc

956 j SCS| ser rite-chlonte U/- carbonate) schist

-sericite (actinolite?) - chlonte schist /breccia zone

f

Jentina Minefor

A.J. Roy

GEOLOClir AND MINERALIZED STRUCTURES

RESOURCE ASSOCIATES LIMITED

Map No l ; NW Sheet Date : 31 August, 1994Compiled by WilloughbyDrawn by Faltada

Scale . l : 25OOQ 20 4O CO to too